How Natural Disasters Affect Political Attitudes and Behavior: Evidence from the 2010-11 Pakistani Floods∗ C. Christine Fair† Patrick M. Kuhn‡ Neil Malhotra§ Jacob N. Shapiro¶ This version July 27, 2013. Abstract How societies make the transition from autocracy to democracy and then on to functioning programmatic politics is a key concern of scholars in both economics and political science. A number of recent papers have studied the relationship between exogenous shocks – such as natural disasters – and governance as a way of testing how economic conditions affect politicians’ incentives and behavior. Of course, the claim that an observed positive relationship between an exogenous shock and governance reforms provides evidence for economic mechanisms requires that the shock primarily impacts politicians’ incentives through that channel. Using evidence from the 2010-11 floods in Pakistan we show that this claim cannot be sustained for natural disasters, at least not in one critical case. Leveraging diverse data sources (geospatial measures of flooding, election returns, and an original survey of 13,282 Pakistani households), we show that flood exposure led Pakistanis to have more aggressive attitudes about civic engagement, increased both turnout and vote share for the party in power in 2010, and led to a rejection of militant groups and small particularistic parties. In this case a major natural disaster which created a transient economic shock also led to major changes in citizens’ attitudes and civic engagement. These results call into question the interpretation of a broad set of papers and tie into a rich literature in political science showing that disasters can have complicated political effects that are often quite divorced from their economic impacts. ∗ The authors thank Tahir Andrabi, Eli Berman, Graeme Blair, Mike Callen, Jishnu Das, Rubin Enikopolov, Asim Khwaja, Rebecca Littman, Rabia Malik, Hannes Mueller, Maria Petrova, Paul Staniland, Basit Zafar, and seminar participants at the 2013 AALIMS Conference at Rice, the University of Chicago, and Yale for their helpful comments and feedback. All errors are our own. This research was supported, in part, by the Air Force Office of Scientific Research, grant #FA9550-09-1-0314. † Assistant Professor, School of Foreign Service, Georgetown University; Email: c christine fair@yahoo.com. ‡ Pre-doctoral Fellow, Empirical Studies of Conflict Project, Princeton University; E-mail: pmkuhn@princeton.edu. § Associate Professor, Stanford Graduate School of Business; E-mail: Malhotra Neil@GSB.Stanford.edu. ¶ Assistant Professor, Woodrow Wilson School and Department of Politics, Princeton University, Princeton, NJ 08544; Email: jns@princeton.edu. Corresponding author. 1 Introduction How societies make the transition from autocracy to democracy and then on to functioning programmatic politics is a key concern of scholars in both economics and political science. A number of recent papers have looked to the relationship between exogenous shocks – such as natural disasters – and democratization or public goods provision as a way to provide evidence on that process (e.g., Brückner and Ciccone, 2011; Ramsay, 2011; Brückner and Ciccone, 2012). In the economics literature, Brückner and Ciccone (2011) prominently argue that the observed positive relationship serves to test an opportunity-cost mechanism first articulated by Acemoglu and Robinson (2001), in which negative income shocks increase citizens’ willingness to participate in rebellion, which in turn creates incentives for politicians to democratize and provide public goods in order to avoid paying the costs of repression. The idea that natural disasters increase the risks of rebellious behavior has broad empirical support (e.g., Nel and Righarts, 2008; Burke, Hsiang and Miguel, 2013), though it is not uncontested (e.g., Slettebak, 2012). But the claim that an observed positive relationship between natural disasters and governance provides evidence for opportunity cost mechanisms requires that disasters primarily impact citizen behavior (and therefore politicians’ incentives) through the economic channel. That claim is hard to sustain. Correlations between disasters and conflict (or democratization) by themselves provide little direct evidence on the mechanism (Burke et al., 2009) and there is a rich literature showing that disasters can have a wide-range of politically-relevant consequences. In developed countries, researchers have long noted that voters punish politicians for natural events beyond their control (Achen and Bartels, 2004; Healy and Malhotra, 2010), and new evidence suggests they do so in developing countries as well (Cole, Healy and Werker, 2011). Disasters also lead to reactions by governments and other organizations that can shift both citizens’ beliefs and the opportunities for would-be rebels. Andrabi and Das (2010), for example, find that the provision of aid by outsiders in the wake of the devastating 2005 earthquakes in Khyber Pakhtunkhwa (KPK) province and Azad Kashmir led to a substantial increase in trust towards outsiders. Berrebi and Ostwald (2011) show that terrorism increases after natural disasters and that the effect is concentrated among less-developed countries, which they attribute to the twin effects of turmoil after a catastrophe (which could allow militants to exploit the exacerbated vulnerabilities of the state) and 2 the government allocating resources away from maintaining order and towards disaster relief. Using evidence from the 2010-11 floods in Pakistan, we demonstrate that natural disasters can impact a range of politically relevant variables above and beyond citizens’ material well being. The 2010 flood affected more than 20 million people, caused between 1,800 and 2,000 deaths, and damaged or destroyed approximately 1.7 million houses, making it the worst flood in Pakistan’s modern history.1 The 2010 floods were driven by an unusual monsoon storm that dropped historically unprecedented levels of moisture on the mountainous northwest regions of the country. According to government accounts, Khyber Pakhtunkhwa (KPK) received 12 feet of rain from July 28 to August 3, four times the province’s average annual total (Gronewold, 2010). Those exceptionally high rainfall rates in mountainous areas compounded what was already an unusually rapid snowmelt to trigger flash floods that vastly exceeded anything in historical memory. As the water drained from KPK during the first week of August, a more typical monsoon storm inundated the Indus flood plain, rendering it incapable of absorbing the dramatic inflows from the mountainous regions and overwhelming many water-management structures. The following year Pakistan got hit by an unusually strong monsoon storm, causing another round of devastating floods in the southern plains. The surging waters hit some places more than others due in part to the random combination of human action, prior differences in soil moisture, micro-topographic differences, and complex fluid dynamics. We leverage that plausibly exogenous variation and diverse data sources (geospatial measures of flooding, election returns, and an original survey of 13,282 households) to show that Pakistanis living in flood-affected places turned out to vote at much higher rates, that those hit hard by the floods have more aggressive attitudes about demanding government services, and that they know more about politics. These effects are substantively large. Turnout in the Pakistani national and provincial elections rose roughly 11 percentage points between 2008 and 2013 (from 44% to 55%), a massive increase. Our results suggest that approximately 19% of this change can be attributed to the impact of the 2010 floods.2 Put differently the increased civic engagement due to the floods led to a 2 percentage point change in the absolute level of turnout.3 We also find modest evidence 1 The EM-DAT International Disaster Database records approximately 20.4 million people affected and 1,985 killed from the 2010 floods. 2 The 95% confidence interval on this effect ranges from 7% to 31% of the change. 3 This is almost half the 5.4 percentage point increase between the 2000 and 2004 U.S. presidential elections and is larger than the 1.4 percentage point increase in turnout in the United States between 2004 and 2008, typically 3 that voters rewarded the government for what was generally considered to be an effective response compared to previous floods in Pakistan.4 While the incumbent Pakistan Peoples’ Party (PPP) lost massively in the 2013 election, losing 16.5 percentage points of vote share in the average constituency, their loses were roughly 25% smaller in flood-affected constituencies. Voters in floodaffected areas also turned away from small particularistic parties and became less supportive of a range of militant groups. We find no evidence that these results were driven by patronage goods distributed differentially to flood-affected areas (or that if there was patronage in the guise of flood relief it did not work). Overall, this major natural disaster, which clearly created a transient economic shock, also led to major changes in citizens’ attitudes and civic engagement. These results call into question the interpretation of a broad set of papers and tie into a rich literature in political science showing that disasters can have complicated political effects that are often quite divorced from economic impacts. Our results also speak to three additional literatures. First, this paper advances the broad literature on the political impact of natural disasters on two distinct fronts. Researchers studying whether voters objectively evaluate politicians’ performance and respond accordingly have become increasingly interested in how voters react to natural disasters because their occurrence is exogenous to politicians’ actions.5 Achen and Bartels (2004), for example, find that extreme droughts and floods cost incumbent U.S. presidents about 1.5 percentage points of the popular vote. They theoretically interpret this empirical pattern as an example of “blind retrospection,” or voters failing to hold leaders accountable only for conditions over which they have direct control and responsibility. Healy and Malhotra (2010) similarly find that heavy damage from tornadoes decreases presidential vote share by about 2 percentage points. Subsequent studies have found that voters may in fact be reacting to the government’s actions in responding to the disaster, suggesting that citizens sanction elected officials only when they fail to adequately address the negative effects of disasters (Gasper and Reeves, 2011). For instance, politicians are rewarded for providing relief payments in the wake of a disaster (Healy and Malhotra, 2009; Bechtel and Hainmueller, 2011; Cole, Healy and Werker, 2011) or even for providing distributive spending under the guise of relief efforts (Chen, 2013). attributed to an unusually motivated electorate turning out in support of a historic candidacy. 4 The government was particularly effective at coordinating the large flows of foreign aid. 5 Though not their consequences, of course. 4 With a few exceptions this research is built on studies of the effect of natural disasters in advanced developed democracies, a gap we help to fill by focusing on a young developing democracy with weak democratic institutions and active militant groups.6 In addition, the vast majority of these studies focuses on the political outcome of this exogenous event (e.g., Lay, 2009; Reeves, 2011; Velez and Martin, 2013) ignoring the underlying causal mechanism. Ours is the first study we know of which measures political attitudes in the period between a highly salient natural disaster and a subsequent election. This enables us to measure how the flood impacted attitudes relevant to interpreting the electoral outcome in the disasters aftermath. Consequentially, we shed light on the mechanism through which disasters affect elections. Second, we provide valuable evidence on the question of what drives governments from patronclient systems—which focus on providing targeted benefits to supporters at the cost of services with larger collective benefits—to programmatic systems focused on effective service provision. Most work on subject has focused on elite bargaining and left unexamined how changes in citizens’ preferences impact elite incentives (e.g., Shefter, 1977; Acemoglu and Robinson, 2012). Yet, as Besley and Burgess (2002) show theoretically and empirically, more informed and politically active electorates create strong incentives for governments to deliver services.7 The evidence from Pakistan, a country long considered a stronghold of patronage politics, suggests that exogenous events can create just such changes in the electorate. Situated on a range of geo-political fault lines and with a population of more than 180 million people, scholars and analysts variously describe Pakistan as a struggling military-dominated democracy, a revisionist nuclear power locked in a security competition with a nuclearized India, and a failed or failing state (Ziring, 2009; Narang, 2013; Shah, 2013). The 2013 elections there were the first time a freely elected parliament served its term and handed power to another elected government. It was, in other words, the first time that voters were able to punish/reward politicians in something even remotely close to the democratic ideal.8 And those hit hard by a natural disaster years before the election used that opportunity to vote at higher rates and to reward a government that exceeded almost all expectations about how 6 The main exceptions are Cole, Healy and Werker (2011); Gallego (2012); Remmer (2013). Pande (2011) provides a review of experimental evidence showing that providing voters with information improves electoral accountability. 8 The latter was a result of the galvanized public, as evidenced by unprecedented and diverse (gender, age, education) voter turnout, the rise of a competitive third party, and numerous highly contested races in previous one-party strongholds. 7 5 well it would respond (relative to the national trend, of course). Such changes augur well for the emergence of programmatic politics and suggest the theoretical literature should explicitly consider the conditions under which such changes lead to differences in actual policies. Finally, our results are relevant to the emerging literature on the impact of natural disasters on conflict. Scholars in this literature typically find a positive relationship between natural disasters and conflict (see e.g. Miguel, Satyanath and Sergenti, 2004; Brancati, 2007; Ghimire and Ferreira, 2013), though there are exceptions (Berghold and Lujala, 2012). These findings worry many as climate change is predicted by most models to lead to a long-run increase in the incidence of severe weather-related disasters (Burke, Hsiang and Miguel, 2013). The evidence from Pakistan suggests that effective response to such disasters can mitigate their negative political impact. In this case, the international community provided a great deal of post-disaster assistance which the state effectively coordinated. The net result was a differential increase in civic engagement by citizens in flood-affected regions. The results thus provide micro-level evidence that aid in the wake of natural disasters can turn them into events which enhance democracy, a possibility consistent with the cross-national pattern identified in Ahlerup (2011) who finds that natural disasters are correlated with democratization in countries that are substantial aid recipients.9 The remainder of this paper proceeds as follows. Section 1 provides the relevant background on the 2010 Pakistan floods. Section 2 describes our various data sources. Section 3 outlines how we measure key variables. Section 4 describes our strategy for data analysis. Section 5 presents the results. Section 6 conclude by providing a theoretical interpretation of our results, discussing policy implications, and laying out directions for future research. 1 Background on the Pakistan 2010 Flood As the flood waters swept through the province of Khyber Pakhtunkhwa (KPK) and into Punjab in the summer of 2010, journalists reporting on Pakistani politics worried the unfolding disaster would be a boon for militant organizations. Militant organizations played into this concern, with a Tehrik-i-Taliban Pakistan (TTP) spokesman famously offering to contribute $20 million to the relief effort if the Pakistani government would eschew any Western aid (Associated Press of Pakistan 9 Note, this interpretation is not consistent with the theoretical arguments that aid flows increase the risk of conflict by increasing the rents to be captured from control of the government (Besley and Persson, 2011). 6 (APP), 2010). Typical headlines at the time described a situation in which militants could step in and win loyalty by providing badly needed services: • “Militant groups have 3000 volunteers working around the country.” Christian Science Monitor, August 6. • “Pakistani flood disaster gives opening to militants.” Los Angeles Times, August 10. • “’Hardline groups step in to fill Pakistan aid vacuum.” BBC News, August 10. • “Race to provide aid emerges between West and extremists.” Der Spiegel, August 16. • “Pakistan’s floods: a window of opportunity for insurgents?” ABC News, September 8. The scale of the disaster dwarfed anything in recent memory. The 2010 floods affected more than 20 million people (i.e., about 11% of the total population), temporarily displaced more than 10 million people and killed at least 1,879, with the 2011 floods affecting another 5 million, displacing another 660,000 people, and killing at least 5,050 more (Dartmouth Flood Observatory (DFO), 2013; Center for Research on the Epidemiology of Disasters (CRED), 2013). A survey of 1,769 households in 29 severely flood-affected districts found that 54.8% of households reported damage to their homes, 77% reported at least one household member with health problems, and 88% reported a significant household income drop (Kirsch et al., 2012). Figure 1 shows exactly how much of an outlier the 2010 floods were within Pakistan’s flood history. Both graphs show standardized values for the number affected, displaced, and killed for each flood between 1975 and 2012. The upper graph uses data from the International Disaster Database (EM-DAT) hosted by the Center for Research on the Epidemiology of Disasters (2013) (data range 1975-2012) and the lower graph draws on data from the Global Active Archive of Large Flood Events of the Dartmouth Flood Observatory (DFO) (2013) (data range 1988-2012). In terms of the number affected and the number displaced, the 2010 floods were the largest in the modern history of Pakistan by several orders of magnitude and according to the EM-DAT almost twice as devastating as the next largest flood.10 For comparison, Hurricane Katrina killed 1,833 people in the Gulf Coast in 2005 even though many fewer people were directly affected; approximately 500,000 according to the EM-DAT database. INSERT FIGURE 1 HERE 10 The next largest was the 1992 flood which affected 12.8 millions, displaced 4.3 million, and killed at least 1,446 people. 7 The 2010 floods also led to an unprecedented reaction by Pakistani civil society; the central, provincial, and district governments; as well as by the international community (Ahmed, 2010). The overall leader for donor coordination was Pakistan’s Economic Affairs Division while Pakistan’s National Disaster Management Agency (NDMA) which directed and coordinated the various relief efforts. The NDMA maintained close working relationships with relevant federal ministries and departments, Pakistan’s armed forces, and donor organizations supporting the relief efforts to ensure that resources were mobilized consistent with local needs. At the provincial level, the chief minister of each province was responsible for ensuring that various line ministries and the Provincial Disaster Management Authorities acted in concert with each other and with the international and domestic relief efforts. At the district level, district coordination officers were responsible for those activities of local governance that are devolved to the district level (Office for the Coordination of Humanitarian Affairs (OCHA), 2010; National Disaster Management Agency, 2011). This complex system often made it difficult to discern who was responsible for success or failure. In December 2010, one of the authors visited two relief camps, one each in Nowshera (KPK) and Dadu (Sindh). The Pakistan military was most visible through their air, road and water missions by uniformed personnel. Tents and other supplies were usually branded by the donor (e.g., the United Nations, US AID, etc.), but the distribution of these goods was done through Pakistani personnel. This was often deliberate as the intention of many donor and bilateral organizations was to foster the impression that the Pakistani government was effectively managing relief efforts.11 In addition, there were spontaneous localized self-help efforts that emerged during the initial phase of the crisis and continued throughout. These included victims and their kin’s own efforts to save their belongings but also included survivor-led repair of local access roads and bridges after the floods receded. This was in addition to an enormous civil society response that tended to spontaneously coalesce at very local levels (mohallas, union councils, villages, etc.). Such local groups collected and distributed truckloads of relief items. Countless local as well as national organizations set up collection sites for donations of goods and cash and then undertook the distribution of the same. Individual philanthropists, professional bodies, and even chambers of commerce donated money and supplies to the victims. Scholars associated with Pakistan’s Sustainable Development Policy Institute note the importance of these local forms of assistance but contend that they are 11 Author fieldwork in Nowshera and Dadu in December 2010 and January 2011. 8 virtually unknown (and thus poorly documented) beyond the local level (Shahbaz et al., 2012). Such volunteerism was not unique to the 2010 flood; rather, it is a common feature in Pakistan’s domestic response to such calamities. Halvorson and Hamilton (2010), for example, document extremely high levels of volunteerism following the 2005 Kashmir earthquake.12 By the end of July 2010 the government had appealed to international donors for help in responding to the disaster, after having deployed military troops in all affected areas together with 21 helicopters and 150 boats to assist affected people (Khan and Mughal, 2010).13 In response, the United Nations launched its relief efforts calling for $460 million to provide immediate help, such as food, shelter, and clean water. Countries and international organizations from around the world donated money and supplies, sent specialists, and provided equipment to supplement Pakistani government’s relief efforts. According to the United Nations Office for the Coordination of Humanitarian Affairs (UNOCHA) (2010), by November 2010, a total of close to $1.792 billion had been committed in humanitarian support, the largest amount by the United States (30.7%), followed by private individuals and organizations (17.5%) and Saudi Arabia (13.5%).14 Government response (both internal and external) dwarfed anything non-state actors could do. Thus, if we believe the state was in a competition over service provision with various militant groups, it should have won hands down.15 The government’s effort and the massive influx of foreign aid made the response quite effective. Calculating the ratio of killed to 1,000 people affected from the EM-DAT data and the ratio of deaths to 1,000 people displaced for each flood between 1975 and 2012 from the DFO data, provides a proxy for the effectiveness of the government’s response. For the 2010 flood, the ratios are 0.10 and 0.19, respectively, which is the smallest ratio in the DFO series (1988-2012) and the seventh smallest ratio in the EM-DAT series (1975-2012).16 Strikingly, the 2010 ratio is only 21% of the median ratio of killed to 1,000 displaced in the DFO data, so roughly one fifth as many people died 12 Note that this is not unique to Pakistan either. Scholars have also noted this elsewhere in South Asia (see e.g., Haque, 2004; Rahman, 2006; Ghosh, 2009). 13 The United States provided an additional seven helicopters as part of their relief efforts. 14 By April 2013, this total has increased to more than $2.653 billion with the three largest donor groups being the United States (25.8%), private individuals and organizations (13.4%), and Japan (11.3%) (UNOCHA, 2013). 15 As Appendix Table 1 shows, respondents were less likely to say militant groups engage in disaster relief efforts if they live in flood-affected areas, though whether this is because these groups were absent or because respondents where the groups did operate do not want to give them credit when talking to our enumerators is unknown. 16 Compared to the 1992 flood, the only flood of comparable magnitude in the last 30 years, the 2010 ratio is 72% smaller when using the DFO data and 8% smaller looking at the EM-DAT data. 9 as would have been expected given the median response in the last 37 years. Compared to previous incidents, the government performance in handling the 2010 floods appears quite good. 2 Data Sources We leverage three main data sources to measure variables of interest: (1) geocoded data on flood exposure to measure the main treatment variable; (2) returns from the 2013 National and Provincial Assembly elections (along with lagged election results) to measure the behavioral outcomes; and (3) an original survey we conducted in early-2012 to measure attitudinal outcomes. 2.1 Geocoded Flood Data Geo-spatial data on the 2010 and 2011 floods come from the United Nations Institute for Training and Research’s (UNITAR) Operational Satellite Applications Program (UNOSAT), which provides imagery analysis in support of humanitarian relief, human security, and strategic territorial and development planning (United Nations Institute for Training and Research, 2003). For the 2010 flood UNOSAT provided a time series of satellite data recorded between the end of July and mid September. For the 2011 flood in Sindh province UNOSAT provided a map of the standing flood waters following heavy monsoon rain between mid-August and early October. Overlapping the various images allowed us to generate a layer of maximal flood extent in the two years prior to the survey data collection at the beginning of 2012. Our spatial population data was taken from Oak Ridge National Laboratory’s (2008) Landscan dataset, which provides high-resolution (1km resolution; i.e., 30” × 30”) population distribution data for 2011. The digital administrative boundary data of all tehsils and electoral constituencies for the national and provincials assembly were developed from constituency-level maps available from the Electoral Commission of Pakistan (ECP) website. 2.2 2013 Election Data We collected election data for the 2002, 2008, and 2013 National and Provincial Assembly elections from the ECP website. The ECP website lists by-election results when a constituency has changed hands due to the death of it’s representative or to him/her shifting to a new job. As by-election 10 contests are likely to have a different dynamic than those held during the general election we replaced as many of the by-election results as possible with the original results from the main polling date. For the National Assembly election, we managed to find general election data on all contests except for five constituencies in 2008. For the Provincial Assembly election, we were able to find polling results from the general elections for all by-elections in 2002 and 2008. For each constituency we recorded turnout as well as the vote shares for all candidates on the ballot. 2.3 The Survey Our survey included a large sample (n=13,282) of respondents in the four largest provinces of Pakistan (Balochistan, Khyber Pakhtunkhwa (KPK), Punjab, and Sindh). We collected districtrepresentative samples of 155-675 households in 61 districts with a modest over-sample in heavily flood-affected districts as determined by our spatial flood exposure data. We sampled 15 districts in Balochistan, 14 in KPK, 12 in Sindh, and 20 in Punjab to ensure we covered a large proportion of the districts in each province. Within each province we sampled the two largest districts and then chose additional districts using a simple random sample. The core results below should be taken as representative for our sample which, while large, does over-represent Pakistanis from the smaller provinces. Weighted results using either sample weights calculated from Landscan gridded population data or those provided by the Pakistan Federal Bureau of Statistics are substantively and statistically similar. Our Pakistani partners, SEDCO Associates, fielded the survey between January 7 and March 21, 2012. Our overall response rate was 71%, with 14.5% of households contacted refusing the survey and 14.5% of the targeted households not interviewed because no one was home who could take the survey. This response rate rivals those of high-quality academic surveys in the United States such as the American National Election Study (ANES). 3 3.1 Measurement Outcome Variables: Civic Engagement We measure three outcomes that tap civic engagement: electoral turnout, attitudes towards using violence as a means of achieving political ends, and political knowledge. 11 Turnout We collected turnout data for the 2002, 2008, and 2013 elections for all 260 constituencies of the National Assembly of Pakistan (excluding FATA constituencies) and the 577 constituencies of the four Provincial Assemblies. Together with those five National Assembly constituencies for which we could not find the original general results, we also dropped all constituencies that were uncontested (i.e., no polling occurred because there was only one candidate), where elections were terminated or re-polling was scheduled in 2013, and where the ECP did not report turnout and it could not be inferred from the information given. This leaves us with 246 out of the 260 (i.e., 95.8%) National Assembly and 560 out of the 577 (i.e., 97.1%) Provincial Assembly constituencies. The Pakistan National and Provincial Assemblies combine members elected in single-member first-past-the-post elections at the constituency level (272 for the National Assembly and 577 for the Provincial Assemblies in the four main provinces) plus a number of seats reserved for women and minorities (70 in the national assembly) that are allocated among parties according to a proportional representation scheme. Most candidates align with a party but some run as independents and affiliate with a party for coalition formation purposes after the election is complete. Candidates in the 2013 election campaigns combined appeals to national issues and party platforms with locality specific appeals and promises of patronage, with the mix varying by candidate. Aggressive Political Action: Vignette Experiment In order to measure support for aggressive political action we use a vignette experiment. This approach circumvents three main challenges to measuring political attitudes. First, respondents may face social desirability pressures to not explicitly support particular views (e.g. aggressive civic protests). Second, concepts such as the political efficacy of aggressive protests are not easily explainable in standard survey questions, but can be illustrated with examples. Third, respondent answers to direct questions may not be interpersonally comparable (King et al., 2004). To overcome these challenges, we wrote two vignettes describing concrete (but fictional) examples of two different ways of getting the government’s attention: peaceful petition or violent protest. Respondents were randomly assigned to receive one of the vignettes before answering the same two survey questions on how effective they think the chosen method is and whether they approve of it. 12 More specifically, the vignette experiment works as follows. At the primary sampling unit (PSU) level, respondents are randomized into one of the following two vignettes: Peaceful Petition. Junaid lives in a village that lacks clean drinking water. He works with his neighbors to draw attention to the issue by collecting signatures on a petition. He plans to present the petition to each of the candidates before the upcoming local elections. Violent Protest. Junaid lives in a village that lacks clean drinking water. He works with his neighbors to draw attention to the issue by angrily protesting outside the office of the district coordinating official. As the government workers exit the office, they threaten and shove them. Following the vignette respondents are asked the following: • Effectiveness. “How effective do you think Junaid will be in getting clean drinking water for his village?” (response options: “extremely effective,” “very effective,” “moderately effective,” “slightly effective,” “not effective at all”) • Approval. “How much do you approve of Junaid’s actions?” (response options: “a great deal,” “a lot,” “a moderate amount,” “a little,” “not at all”) Our sample is well balanced across conditions in the vignette experiment on a broad range of geographic, demographic, and attitudinal variables, as Figure 2 shows. The difference in means between the groups within a region therefore provides an estimate of how effective/acceptable citizens think the use of violence is to pressure their political representatives, which we referred to earlier as a form of unconventional politics. INSERT FIGURE 2 HERE Political Knowledge We construct a simple measure of political knowledge using a set of binary questions. To tap awareness of political issues, we asked respondents whether they were aware of four policy debates 13 that were prominent in early-2012: whether to use the army to reduce conflict in Karachi; how to incorporate the FATA into the rest of Pakistan; what should be done to resolve the disputed border with Afghanistan; and whether the government should open peace talks with India. To capture political knowledge, we asked six questions about politicians and scored whether respondents correctly identified the following: who led the ruling coalition in Parliament (the PPP); and the names of the President, Prime Minister, Chief Minister of their Province, Chief of Army Staff, and Chief Justice of the Supreme Court. Following evidence in Kolenikov and Angeles (2009) we conduct principal component analysis on the polychoric correlation matrix of these items and use the first principal component as our measure of political knowledge. That component accounts for 49.15% of the variance in the index of ten components, suggesting it does a good job of capturing our underlying concept. 3.2 Outcome Variables: Government and Militant Support We measure two outcomes that tap government support: vote shares for the ruling party in the 2008 and 2013 elections as well as support for a range of violent non-state militant groups that may have served as substitutes for the government. Incumbent Vote Share Measuring vote shares is straightforward as described above. There were a number of reports of fraud in the 2013 election, but most were concentrated in urban Karachi and none of the major observers reported widespread or systematic vote fraud. Ultimately, vote fraud would affect our inferences on government support to the extent that it was spatially correlated with flood impacts, which appears highly unlikely given available evidence. Support for Militant Groups: Endorsement Experiment We also measured support for some of the violent non-state groups that are a key element of Pakistani politics. The floods’ affects on support for militant groups was a prime concern of many policy actors (Varner, 2010), and that support also provides a proxy for disaffection with normal politics. 14 Drawing on an approach used in a range of papers studying sensitive attitudes in Pakistan and Afghanistan we employ an endorsement experiment to measure attitudes towards militant groups (Blair et al., 2012; Blair, Lyall and Imai, 2013).17 The goal of the endorsement experiment is to measure support for militant groups without asking respondents directly about them. In a place like Pakistan, direct questions on violent groups are subject to social desirability bias, have extremely high rates of non-response, and threaten the safety of enumerators, particularly in rural areas where militant groups are active. In an endorsement experiment, the difference in respondents’ evaluations of a policy is compared when they are presented with the policy alone and when they are told the policy is supported by a specific group. The difference in means between the two groups is the measure of affect towards the endorsing actor. We measured support for three militant groups—Sipah-e-Sahaba Pakistan (SSP), the Pakistan Taliban, and the Afghan Taliban.18 Using a five-point scale ranging from “not at all” to “a great deal” we asked respondents how much they support policies which were relatively well known but about which they do not have strong feelings (as we learned during pretesting). In this case we randomized equal proportions of the respondents into treatment conditions in which they are told that one of the actors mentioned above supports the policies in question. The only difference between the treatment and control conditions is the group endorsement. The list of policies respondents were asked about were: • Whether to use the army to deal with the violence and extremism in Karachi; • Whether to make FATA a part of KPK and extend Pakistan’s constitution to this area; • Whether to use peace jirgas to resolve boundary disputes with Afghanistan; and • Whether the Pakistani government should continue engaging India in a dialogue to resolve their differences. As with the vignette, our sample in the endorsement experiment is well-balanced on a broad range of geographic, demographic, and attitudinal variables, as Figure 3 shows. 17 See Bullock, Imai and Shapiro (2011) for a measurement theory justification of this approach. SSP is a sectarian militant group that mostly targets the Shia minority in Pakistan. The Pakistan Taliban is an umbrella label for an array of Pashtun militant organizations all of which advocate for some combination of Islamist governance and regional autonomy in the Federally Administered Tribal Areas (FATA). The Afghan Taliban are fighting an insurgency against the American-backed government in Afghanistan and are commonly understood to operate out of the border regions of Pakistan. 18 15 INSERT FIGURE 3 HERE There is minor imbalance due to chance on gender, education, and literacy in the endorsement experiment, which we address by controlling for those variables in our core specification (Gerber and Green, 2012). 3.3 Treatment Variable: Flood Impact Figure 4 shows the combined maximum flood extents in 2010 and 2011 overlaid on a map of Pakistan. The 216 tehsils in which we surveyed are highlighted in grey.19 As one can see the surveyed areas include tehsils that were severely impacted, tehsils that had only small portion of their territory affected, and those that were spared by the floods. As described below, we exploit the randomness inherent in flood exposure to identify the impact of the 2010 and 2011 floods on the variables described in the previous section. INSERT FIGURE 4 HERE We measure flood exposure with two different sets of variables: (1) objective measures based on geo-spatial data; and (2) subjective measures asked of respondents as part of the survey. Objective Measures We calculate objective measures of flood exposure for each of the 409 tehsils, each of the 272 singlemember constituencies for the national assembly, and each of the 577 single-member provincial assembly constituencies using a combination of: geo-spatial data on the maximum flood extents in 2010 and 2011 derived from overhead imagery by the UNOSAT project (http://www.unitar.org/unosat/); high-resolution spatial population data; and a digital map of tehsil and national assembly constituency boundaries. Based on these three input datasets we calculated two different objective measures of flood exposure at the tehsil and constituency level: the percent of area flooded and the percent of population exposed. Based on the population measure we also created two dichotomous variables; one indicating whether at least 5% of a tehsil’s or electoral constituency’s population was exposed 19 The tehsil is the third level administrative unit in Pakistan, below provinces and districts. 16 to the flood (roughly the 50th percentile of all tehsils and electoral constituencies exposed) and the other indicating whether at least 40% of a tehsil’s or or electoral constituency’s population was affected by the floods (roughly the 90th percentile of all tehsils and electoral constituencies exposed). As each method of assessing flood impacts entails some error we report all results for multiple different measures. These objectively calculated variables underestimate the floods’ impacts in steep areas where the floodwaters did not spread out enough to be identified with overhead imagery but where contemporaneous accounts clearly show there was major damage in river valleys. In Upper Dir district in KPK, for example, the UNOSAT data show no flooding but contemporaneous media accounts and survey-based measurements clearly indicate the floods did a great deal of damage to structures that were place well above the normal high-water mark but still close to rivers (see e.g. Agency for Technical Cooperation and Development, 2010). Note that under the null that the floods impacted citizen attitudes this kind of measurement error will attenuate our estimate of flood impacts because we are counting places as having low values on the treatment where the floods actually had substantial effects. Subjective Reports To exploit variation in flood impacts at the household level, we also asked respondents how the floods impacted them. In the analysis below, we use the following question to measure respondents’ subjective assessments of flood damage: “How badly were you personally harmed by the floods?” (response options: “extremely badly,” “very badly,” “somewhat badly,” “not at all”) In addition to treating these responses as an ordinal variable, we created two dichotomous variables of subjective flood exposure: one indicating whether a household was at least “somewhat badly” affected and the other indicating whether a household was at least “very badly” affected. Responses to this question correlate well with other self-reported measures. We asked respondents to rate how much money they lost as a result of the floods on an ordinal scale: less than 50k Pakistani Rupee (Rs.), 50k Rs. to 100k Rs., 100k-300k Rs., and more than 300k Rs. The Pearson correlation between that loss and the subjective measure above is quite high (r = .73). 17 We further measured the relationship between self-reported flood impacts and three measures of current economic outcomes: an asset index constructed from the household’s possession of 24 goods not specific to agricultural production (cell phones, chairs, televisions, motorcycles, etc.), monthly household income, and monthly household expenditures.20 All three are negatively correlated with self-reported flood harm, even after controlling for a rich set of variables related to economic outcomes including tehsil fixed-effects, education, gender, literacy, numeracy, and whether the respondent was the head of the household. As Appendix Table 2 shows, a one-point increase in the four-point self-reported harm scale is associated with a .39 s.d. reduction in the asset index, a .14 s.d. reduction in log monthly income, and a .10 s.d. reduction in log monthly expenditures. In the short run, we would expect the floods to have a significantly greater destructive impact on household assets than human capital. The comparatively larger reduction in household assets is thus just what we should expect if self-reported flood exposure is honest and accurate. Over the 1.5 years between the flood and our survey we could expect that rebuilding income would be easier than regaining all pre-flood assets, especially given the absence of flood insurance and the bumper crop Pakistan experienced following the floods which stabilized the rural economy (Looney, 2012). 4 Methodology and Research Design This section describes our identification strategy, the statistical models we estimate, and the control variables included. We first discuss our approach to estimating the floods’ effects on individual outcomes—support of using more violent means to achieve government responsiveness, political knowledge, and affect towards non-state militant groups—and then how we modify that strategy to study the flood’s impact on aggregate-level outcomes—turnout and electoral behavior. 4.1 Individual-Level Outcomes: Political Knowledge, Vignettes, and the Endorsement Experiment Our identification strategy at the individual level is to use district fixed-effects and respondent-level controls to isolate the effect of local variance in flood impact that is unrelated to average flood risk. We demonstrate that: (1) selection on unobservables would have to be unrealistically large to be 20 We omit assets related to agricultural production as many aid efforts provided help rebuilding those assets. 18 generating the main effect; and (2) the results are consistent across subsets of the data over which the presence of likely confounders should vary a great deal. Specifically, when we compare places that were similarly likely to be affected by the 2010 flooding due to proximity to rivers, some of which were badly damaged and others spared, our core results remain consistent. For the political knowledge index our estimating equation is a fixed-effect regression Yi = α + β1 Fi + γd + BXi + i , (1) where Fi is one of our flood exposure measures, γd is a district fixed-effect, and Xi is a vector of demographic and geographic controls to further isolate the impact of idiosyncratic flood effects by accounting for the linear impact of those variables within tehsils. We cluster standard errors at the PSU level. For the vignette experiment our measurement approach leverages a difference-in-difference estimator to answer a simple question: given that people are generally opposed to the pro-violence vignette, is the difference in reactions between the pro and non-violence vignettes smaller for people in areas exposed to the flooding? To answer that question we need to control for a range of potential confounders. For example, we might worry that in districts close to rivers (which are most likely to be flooded), people are generally more accepting of violence because that location is less desirable and so people living there tend to be poorer and more marginalized. It actually seems unlikely that land near the rivers is undesirable; it is more fertile and population density is substantially higher near major rivers. But, that then raises the concern that people more likely to be affected would tend to be wealthier and less marginalized. In either case, we risk confounding flood exposure with a more fixed characteristic of the region and the people who reside there, a challenge given that we have survey data from a single cross section. We therefore estimate the following as our core specification for analyzing the vignette experiment: Yi = α + β1 Vi + β2 Fi + β3 (Vi × Fi ) + γd + BXi + i , (2) where i indexes respondents, Yi represents a response to either the effectiveness or approval variable, Vi is an indicator for whether an individual received the protest vignette, Fi represents a 19 respondent’s flood exposure (either objective or self-reported), γd represents a district fixed effect intended to capture regional differences in baseline propensities to express approval or perceived effectiveness, and Xi is a vector of demographic and geographic controls to further isolate the impact of idiosyncratic flood effects.21 We again cluster standard errors at the PSU level since that is the level at which the vignette was randomized.22 The estimate of β3 in these equations isolates the causal impact of the flood to the extent that: (1) which vignette a respondent got was exogenous to their political attitudes; and (2) how exposed one was to the floods depended on factors orthogonal to pre-existing political factors once we condition on district-specific traits and the geographic controls. The first condition is true due to random assignment of the survey treatment. The second condition is likely to be met for the reasons outlined above. At the individual level, we can also exploit variation in flood effects at the household level. Both our discussions with those involved in flood relief and surveys done to assess post-flood recovery needs show there could be huge variation in damages suffered at the household level (Kurosaki et al., 2011), likely due to minor features of topography that impacted flow rates, how long areas were submerged, and so on. For the endorsement experiment, we estimate a similar specification as equation (3): Pi = α + β1 Ei,j + β2 Fi + β3 (Ei,j × Fi ) + γd + ∆Xi + i , (3) where Pi represents average policy support and Ei,j is a dummy variable for whether the individual was told that the policy was endorsed by group j ∈ {Sipah-e-Sahaba Pakistan (SSP), Afghan Taliban, Pakistan Taliban}. In addition, we estimate an endorsement effect average across the militancy groups by pooling together all respondents who received endorsements from militant groups, in which case Ei,j = 1 for all respondents who received a militant group endorsement. Additionally, we conduct a number of robustness checks to enhance the plausibility of our claim that we have isolated the impact of the exogenous component of the floods. First, we show 21 Geographic controls that enter at the tehsil level include distance to major river from the tehsil centroid, a dummy for bordering a major river, the mean elevation of the tehsil, the standard deviation of elevation within the tehsil, and the proportion of the population hit by the 2011 floods that occurred after 2010 but before our survey was fielded. Respondent-level demographic controls include gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy (measured by a basic mathematical task), and level of education. 22 Results are robust to clustering at the district level to account for the high possibility that the variance attitudes is highly correlated within districts as well as within PSUs. 20 that selection on unobservables would have to be unrealistically large relative to observables to fully account for the result. Second, we restrict our analysis to tehsils alongside rivers as doing so effectively compares places that were roughly similar ex ante in terms of the threat of flood exposure. 4.2 Aggregate-Level Outcomes: Turnout and Incumbent Vote Share Our identification strategy at the constituency level relies on a combination of fixed-effects and constituency-level geographic controls to isolate the impact of local variation in flood intensity on electoral turnout. In doing so, we need to control for a range of locality-specific confounders. We might worry, for example, that it is easier for politicians to deliver patronage to constituencies close to rivers (which are most likely to be flooded) through a combination of water-management projects and prior flood relief, making them more likely to turn out. To avoid confounding flood exposure with more fixed characteristic of constituencies we estimate the following two equations: ∆y2013,2008 = α + β1 Fi + γd + BXi + i (4) ∆y2013,2008 − ∆y2008,2002 = α + β1 ∆Fi + BXi + i , (5) where Fi is a measure of flood impact and ∆Xi is a vector of geo-spatial controls (i.e., distance to major river from the constituency centroid, a dummy for constituencies bordering major rivers, mean constituency elevation, and standard deviation of constituency elevation) plus the proportion of population affected in the smaller 2012 floods that occurred after our survey data collection but before the 2013 general elections. γd is a unit fixed-effect for the division, a defunct administrative unit that was larger than the district but smaller than the province. We control for the 27 divisions instead of districts because outside of Punjab, National Assembly constituencies are often aligned with district boundaries or contain multiple districts. We also estimate the same equations using turnout in the provincial elections which have roughly twice as many constituencies, and the results become substantively and statistically stronger. The geo-spatial controls plus division fixed-effects account for 72.2% of the variance in the area flooded among National Assembly constituencies and 72.4% of the variance in population affected (and slightly less for the Provincial Assembly 21 constituencies at 64.2% and 66.2% respectively). We cluster standard errors at the district level to account for the high probability that the cross-constituency variance in turnout changes may be quite different across districts. Our estimate of β1 identifies the impact of the floods to the extent that how exposed one was to the floods depended on factors orthogonal to pre-existing political factors once we condition on district-specific traits and the geographic controls. That condition seems likely to be met given two facts. First, some areas were flooded due to unanticipated dam/levee failures (some intentional by upstream and downstream land owners, others not) (e.g., Waraich, 2010). Second, the two most readily observable indicators of flood risk are distance to major rivers and elevation. We surely account for a large portion of the residual within-division differences between those who live in a flood plain and those who do not by controlling for the linear impact of those variables. Subject to our identifying assumptions, the first equation measures whether there are any systematic changes at the constituency level between 2008 and 2013 associated with flood exposure. The second specification checks whether the trends in turnout shift differentially in flood-affected constituencies, effectively removing constituency-specific factors via differencing. Since the main threat to identification here comes from location-specific trends in the political environment that might be correlated with proximity to rivers, and not to time-invariant district-level political factors which we could account for with fixed effects, equation (2) is our preferred specification. Subject to the assumption that there was no major flood event between 2002 and 2008 (which there was not), it effectively differences out all constituency-specific trends.23 We also test the robustness of the second specification to adding a division fixed effect to account for level differences in the change across divisions. 5 5.1 Results Summary Statistics and Randomization Checks Table 1 provides summary statistics for our key treatment and control variables. While slightly more than 8% of the land area in our survey tehsils were flooded on average, those which were 23 We are currently coding satellite imagery on floods back to 2000 so that we can fully include observed flood exposure for prior years in our first-differenced regressions. Since the flooding prior to 2010 was modest we believe that doing so is unlikely to change the results. 22 exposed to the floods were substantially affected. Among the 22% of surveyed tehsils with above median flood exposure in terms of population, the median tehsil had 18% of its population impacted and the average percent of the population affected was almost 25%. INSERT TABLE 1 HERE 5.2 Civic Engagement We measure both behavioral and attitudinal indicators of civic engagement. Attitudinally we study how the flood affected citizens attitudes towards engaging with government and their level of political knowledge. Behaviorally we assess the impact of the floods on turnout. Aggressive Political Action: Vignette Experiment As shown in Table 2, respondents experiencing the economic shocks of the floods were more likely to approve of violent political activity and to believe such activity to be efficacious. The estimate of β1 measures the difference in the outcome variables between the pro-violence and non-violence vignettes for people who scored a zero on the flood exposure measure. As shown in the top row of Panel A, those who received the pro-violence vignette but did not experience flooding rated the effectiveness of Junaid’s actions between .2 and .25 lower in the violent vignette on a 0-1 scale controlling for a broad range of geographic and demographic controls, which is a movement of more than .5 s.d. in all models. This is the case for the various objective measures of flooding (columns 1-4) and the self-reported measures (columns 5-7). We find results of similar magnitude for the approval dependent variable (see Panel B of Table 2). INSERT TABLE 2 HERE Across a broad range of observational and self-reported measures, however, exposure to the flood substantially and significantly lessened this disapproval. The estimate of β1 + β3 in the models tells us the effect of the violent vignette among those highest on the flood index score and the estimate of β3 indicates the moderating effect of flood exposure on the effect of the vignette. A one s.d. movement in the proportion of the population exposed in tehsils with non-zero flood exposure (.17) corresponds to a .16 s.d. increase in perceived effectiveness of the violent action and a .18 s.d. increase in approval for the violent approach. 23 To benchmark these results consider the relationships between the vignette response and gender. Existing research has shown that men are on average more likely to have pro-violent attitudes in the context of normal social relations (Funk et al., 1999) and tend to have more extreme views in some political settings involving violent contestation (Jaeger et al., 2012). The difference in perceived effectiveness of the pro-violence vignette between men and women is approximately .08, which equates to a .2 s.d. movement in effectiveness, and the difference in approval is of similar size (i.e., .07). The difference between those affected by the flood and those who were not in terms of approval is thus slightly smaller than the gender difference in the approval of violent action. The gender difference in perceived effectiveness and approval across the two conditions is even smaller, roughly .06 for effectiveness and .04 for approval, both of which are substantially smaller than all the flood coefficients.24 Drawing on prior work we can also compare the flood affects to differences across attitudes towards Islamist militants’ political positions. As in Fair, Malhotra and Shapiro (2012) we measured individuals’ support for five political positions espoused by militant Islamist groups and combined these in a simple additive scale ranging from 0 to 1. Moving from 0 to 1 on this scale equates to a .21 increase in approval for the violent vignette and a .11 increase in effectiveness. The impact of a one s.d. move in flood exposure is similar in terms of approval to that from going from agreeing with none of the Islamist policy positions to agreeing with all five (and is much larger on the effectiveness measure), which implies it is a substantial shift. Interestingly, the results are not a proxy for satisfaction with flood relief. We asked respondents “In your opinion, did the government do a good or bad job in responding to the floods after they occurred?” on a four-point scale ranging from “very bad” to “very good” with no midpoint so respondents were forced to assign a direction to their views of the government response. As Appendix Table 4 shows respondents’ feelings about the violent vignette are not consistently correlated with how respondents believe the government did in responding to the floods. For some measure of flood effects the dif-in-dif is larger among the 6,158 respondents who felt the government did a poor job of responding to the floods (about 50% of the sample), while for others it is higher among the 6,149 respondents who felt the government did a good job. Clearly we cannot interpret the lack of a difference as falsifying a causal relationship between the quality of government response and attitudes on the vignette. Individuals who rate the government response poorly may do so because 24 To see how the coefficient estimate β̂3 changes based on different sets of control variables, see Appendix Table 3. 24 they have some unobservable difference that also makes them more approving of violent protests to gain political services. Nevertheless, the fact that there is no consistent correlation suggests that the floods affected attitudes (and observable measures of civic engagement as we will see) through some channel other than satisfaction with government performance. The finding that flood victims approve of violent protests and believe they are more effective in getting a government response is quite robust. One might be concerned, for example, that there is unobserved heterogeneity between tehsils which is driving these results. To account for this possibility and to exploit the substantial within-village variation noted by many observers (Kurosaki et al., 2011), we estimated the impact of self-reported flood measures including tehsil fixed effects. As Table 3 shows, the results on self-reported flood effects actually become stronger once we account for tehsil-level variance in flood impacts. INSERT TABLE 3 HERE A second concern is that some enduring attitudinal difference between those who live in flood plains and those who do not may be driving the results. Though this seems unlikely to be the case given the results in Table 2, we estimated our core specification from Table 2 on the subset of 81 tehsils that border major rivers.25 The results in Table 4 are thus identifying off differences in the specific course of the 2010 and 2011 floods among a set of places that are all unambiguously within potential floodplains. Comparing what we can think of as lucky tehsils (i.e., those neighboring rivers, but not flooded) with the unlucky ones (i.e., those neighboring rivers that were hit by the flood) produces somewhat larger estimates of the flood effect than when we include the 103 tehsils that do not border major rivers. This finding provides strong evidence that the result is not driven by the proximity to rivers. INSERT TABLE 4 HERE One might also be concerned that district fixed effects only account for traits correlated with the average response across the two vignette conditions, not for district-specific differences between them. When we include district-vignette fixed effects to allow each district to have a different response in each vignette condition, the core results are attenuated for some measures of flood 25 Major rivers include the Indus river and its arms (i.e., Chenab, Jhelum, Kabul, Ravi, Soan, and Sutlej). 25 impact, but the linear effect of the population proportion affected becomes substantively larger, all coefficients remain positive, and two of three self-reported measures remain statistically significant (see Appendix Table 5).26 Another worry is that what we have identified with the observationally based flood measures is a compositional effect; in other words, those who are not willing to press the government hard moved out of areas after the floods. This is unlikely to be driving our results. If it were, the results should be statistically stronger using the observational measures than the self-reported measures, which are not subject to this compositional bias. The opposite is the case. Moreover, there is little evidence of large-scale migration to or from flood-affected areas. The floods clearly caused some short-term displacement – focusing on 29 “severely” flood-affected districts Kirsch et al. (2012) found that 6 months after the floods 12.6% of urban respondents and 18.4% of rural ones were living outside their home districts – but we could not find evidence this led to long-term movements. In a recent study Mueller, Gray and Kosec (2013) find little evidence that flooding lead to long-term migration in Pakistan. Finally, we can also benchmark how large any unobserved factors linking flood exposure to the attitudes we measure would have to be in order to fully account for the results using techniques from Altonji, Elder and Taber (2005). They suggest gauging how strong selection on unobservables would have to be relative to selection on observables to account for the full estimated effect.27 The measure is calculated using two regressions: one with a restricted set of control variables and one with a full(er) set of controls. Denote the estimated coefficient of interest in the first regression β̂ R , where R stands for Restricted, and the estimated coefficient from the second regressions β̂ F , where F stands for F ull. Their proposed metric is then β̂ F /(β̂ R − β̂ F ). The intuition behind the formula is easy to understand. First, the less the estimate is affected by selection on observables (i.e., the smaller the denominator) the larger the (absolute) ratio and therefore the stronger selection on unobservables need to be (relative to observables) to explain away the entire effect. Second, the larger the absolute value of the numerator is, the higher the ratio is in absolute terms, indicating a greater necessary impact of unobservables to explain the treatment effect away. Third, the relative 26 Note that with district-vignette fixed effects in the model, the vignette-specific mean effect is absorbed. Altonji, Elder and Taber (2005) consider the situation where the explanatory variable is binary. Bellows and Miguel (2009) adapt their test for the case where the variable is continuous. Their derivation of the metric is provided in the working paper of their study, Bellows and Miguel (2008). 27 26 size of β̂ R and β̂ F determines the ratio’s sign. Positive ratios (i.e., β̂ R > β̂ F , as our coefficient estimate of interest is positive) indicates that the added controls attenuated the treatment effect, while negative ratio’s (i.e., β̂ R < β̂ F ) indicate that they increased the treatment effect.28 Negative ratios thus imply that the bias we are removing with the fuller set of controls was pushing towards a null result. Again following Altonji, Elder and Taber (2005) we consider a range of comparisons to provide intuition for the magnitude of the selection on unobservables required to account for the result relative to three intuitive measures: selection on demographic controls at the individual level within district; selection on the combination of geographic and demographic controls within district; and selection on district-specific effects after controlling linearly for geographic and demographic controls. The ratios for these three comparisons across our seven flood treatment variables and both survey questions following the vignette (i.e., effectiveness and approval) are reported in Table 5. INSERT TABLE 5 HERE Of the 42 ratios reported in Table 5, none is between −1 and 1. Including the geographic and demographic controls on top of district fixed effects slightly increases our coefficient estimates (the vast majority of the ratios in the top two rows of each panel are negative). The overall median ratio of −25.21 in these rows suggests that selection on unobservables would have to be very large and push in the opposite direction of the bias we remove by adding geographic and demographic controls to account for the result. Comparing the results with geographic and demographic controls to the results include those controls plus district fixed effects, as we do in the bottom row of each panel, provides a median ratio of 2.76. To attribute the entire flood impact to selection effects, the impact of selection on unobservables within districts would have to be on average more than 2.5 times larger than that of all unobserved district-specific factors. In our view, that makes it highly unlikely that the reported impact of the flood on approval and belief in efficacy of violent protest is due to unobservables. 28 In the knife-edge case when β̂ R = β̂ F the metric is not defined. 27 Political Knowledge Consistent with our interpretation of the floods increasing civic engagement, they also appear to have weakly increased how much citizens know about politics. As Panel A of Table 6 shows, our index of political knowledge is increasing in all our standard measures of flood impact and statistically significantly so in 5 of 7 measures. The effects are generality statistically significant, but small. A one s.d. increase in the proportion of the population affected by the floods (.136) predicts a .062 increase in the knowledge index, a move of .08 s.d.. In order to ensure that the results are not an artifact of the PCA procedure, panel B reports the same regressions with a simple additive index of the 10 knowledge questions. The results are substantively similar. INSERT TABLE 6 HERE Turnout in the 2013 Election The attitudinal changes above were accompanied by a behavioral response. Flood exposure increased electoral turnout, suggesting that these shocks triggered higher demand for government responsiveness. In Panel B of Table 7, our preferred specification, the change in trends for the National Assembly election turnout due to flooding is positive and statistically significant for all objective measures of flood impact. The results are also quite large substantively. A one s.d. increase in the proportion of the population affected by the 2010-11 floods (.127) predicts a 2.1 percentage point higher turnout in 2013 vs. 2008, which is almost a .25 s.d. increase in the outcome (see Panel A, Column 4) and a 3.9 percentage point difference in the trend in turnout (see Panel B, Column 4), roughly a .28 s.d. increase. Comparing Panel B and C in Table 2, we see that the addition of division fixed effects makes most coefficients larger (and the estimates a bit noisier), suggesting the unobserved location-specific factors that are consistent over time are unlikely to be driving the result. These effects are in line with the effects observed in get-out-the-vote campaigns in the United States. Green, Gerber and Nickerson (2003), for example, found that concerted doorto-door canvassing efforts in six sites (areas ranging from 8,000-43,000 people) yielded an average turnout increase of 2.1 percentage points. INSERT TABLE 7 HERE 28 These results remained consistent even when subsetting the data on the 129 electoral constituencies that border major rivers and thus are unambiguously within the flood plain. The results in Panel A of Appendix Table 6 are substantively similar though noisier, as one would expect when the sample size drops from 249 to 129. The results in Panel B, our preferred specification, are almost identical within the restricted subset. The results in Panel C are similar in magnitude for both continuous variables, though a bit less precise, and are substantively smaller for the dichotomous exposure variables, though they retain the same sign and the t-statistics are all above 1. In many countries, voting down ballot is an indicator of intensity of civic engagement as it requires more time in the voting booth and it is harder to collect information on candidates for less prominent offices. In the Pakistan context, voters received two ballots, one for the National Assembly and one for the Provincial Assembly (PA), and turnout in the PA election was 2 percentage points lower (54.1% vs. 56.1%). Examining the impact of floods on PA turnout may thus yield a better signal of the flood’s affects on civic engagement. Moreover, outside of Punjab the National Assembly constituencies are often quite large geographically. Provincial Assembly (PA) constituencies are typically much smaller, there are roughly twice as many across the country. We therefore test the impact of the floods on turnout for PA constituencies as well. As Figure 5 shows, there is substantial variance in flood impacts at the PA constituency level that is masked at the NA constituency level. INSERT FIGURE 5 HERE Given that we have more observations in the PA elections, and that voting there is a clearer signal of civic engagement, it should not be surprising that the results are stronger. As Table 8 shows, a one s.d. increase in the proportion of the population affected by the 2010-11 floods (.146) predicts a 1.6 percentage point increase in 2013 vs. 2008, which is almost a .18 s.d. increase in the outcome (see Panel A, Column 4) and a 3.6 percentage point difference in the trend in turnout (see Panel B, Column 4), roughly a .24 s.d. increase. Comparing Panels B and C in Table 3, we see that the addition of division fixed effects makes most coefficients a bit larger in columns 1 and 2 (and the estimates a bit noisier), suggesting that any unobserved division-specific factors which are consistent over time are unlikely to be driving the result. On average, the flood impact increased turnout in the 2013 PA election by 1.5 percentage points and based on our estimates the flood 29 accounts on average for 14.65% of the turnout increase (with a 95% confidence interval of 6.3% to 22.9%). As before, all results are robust within the subset of constituencies which border major rivers (see Appendix Table 7). INSERT TABLE 8 HERE As before the results are consistent when we restrict attention to the 209 PA constituencies that border major rivers. Our results are clearly not being driven by variance between places that are always at risk and those which rarely are. Is This Just a Compositional Effect? An immediate concern with any results looking at the impact of a natural disaster which are not based on panel data is that we may simply be picking up a compositional effect. If people who moved out after the floods were systematically less likely to vote than those who stayed put (or moved in), then the changes we are attributing to the flood’s impact on individual civic engagement could actually be an artifact of those migration decisions. There in no evidence in surveys designed to study migration that there were significant permanent population shiftings in Pakistan due to the 2010-11 floods, either to or from flood-affected districts (Mueller, Gray and Kosec, 2013). Less than 2% of those reporting their village was hit in the 2010 or 2011 floods in the Mueller, Gray and Kosec (2013) nationally-representative panel study were living in a different village than in 2001.29 Fortunately, our survey provides some evidence on migration, allowing us to provide an estimate of how worried we should be about compositional effects driving our results. A number of respondents reported suffering from flood damage who lived in places that were not affected by the floods in 2010 or 2011 according to the combination of UNOSAT data and maps from the Pakistan National Disaster Management Agency. Of the 1,201 respondents who reported being hurt “extremely badly” by the floods only 75 lived in a tehsil that was not hit by the flood and of the 2,360 who reported being “very badly” or “extremely badly” hit, only 170 live in a tehsil not hit. These numbers are inconsistent with massive outmigration from flood-affected areas. If we assume that all those reporting any damage who live in un-affected districts migrated because of the flood, then we estimate that 4.6% of the population in unaffected districts are 29 Private communication with the authors. 30 migrants from the flood-affected regions and that a total of 2.05% of Pakistan’s population migrated as a result of flood damage. This is surely an overestimate, many of those who report being affected but live in districts with no flooding either moved for other reasons, are referring to damage suffered by kin, or answered based on damage suffered from monsoon rains in the summer of 2010. Still, we can use our estimates of migration to benchmark the difference in turnout attributable to the impact of the flood. The simplest way to do so is to estimate the migration rates for the 61 districts in our survey (recall the sample was designed to be district representative) and add our estimates of the proportion of migrants in a district to our National Assembly turnout regressions. If people who moved out were less likely to vote, then we should see a negative conditional correlation between number of migrants in unaffected communities and the change in turnout from 2008. As Panel A of Table 9 shows, the opposite is the case for National Assembly Constituencies. Instead, the coefficients on migration is positive and insignificant in all regressions. We can also estimate our baseline turnout regression for the 157 NA constituencies that we estimate did not receive any migrants (i.e. they are in districts we surveyed that were either clearly hit by the floods or that had no one report flood exposure). As Panel B shows the core results from Table 7 remain substantially unchanged within that sub-sample. Panel C repeats the analysis of Panel B for the 378 PA constituencies that were either hit or reside in a district where we found no migration. The results from Table 8 remain robust in that subsample. INSERT TABLE 9 HERE We should close this section by noting that the particulars of Pakistan’s voting system mean that compositional changes consistent with the attitudinal results are unlikely to be driving the results. The major door-to-door voter registration effort by the Electoral Commission of Pakistan for the 2013 election occurred from August 22 to November 30, 2011 (mostly after the 2011 floods). Voters were registered at the address on their national identity card and anyone not home during the door-to-door drive could register until March 22, 2013 at their local electoral commission office by providing a national identity card. Because changing the address on one’s national identity card is a relatively cumbersome process (it requires visiting an office with either proof of property ownership or a certificate from a local government representative), many people choose to vote 31 where they were registered rather than shifting that address. This registration process means that if those who moved out were disproportionately inclined not to vote, then their registration would likely remain in flood-affected areas (there would be, after all, no reason for them to shift their registration if they do not plan to vote). That would introduce a downward bias to our estimates of turnout there and therefore introducing a bias against our main result. Overall, there is little evidence that we are detecting a compositional effect, though we cannot rule it out without better information on migration patterns. As we saw above, the attitudinal changes related to flood impacts are consistent across both objectively-measured and self-reported flood exposure, suggesting again that we are not simply capturing the impact of differential migration. 5.3 Government Support Given the broad literature on the impact of natural disasters on voter behavior we examined how the floods affected support for various parties in the 2013 election. Incumbent Vote Share The Pakistan People’s Party (PPP) was the ruling party during the 2010-11 floods. The PPP won 91 out of 272 contested seats in the 2008 election, almost a third more than the second place Pakistan Muslim League (Nawaz) (PML-N) which won 69 seats. In the 2013 election the PPP suffered a massive defeat, winning only 33 seats, while the PML-N scored a massive victory winning 126 seats; almost four times the number of seats of the second-place PPP. Against this background of massive defeat, we ask a simple question: was the PPP’s loss somewhat less stinging in flood-affected constituencies? As Figure 6 shows, they were. We plot the vote share for PPP (Panel A) and PML-N (Panel B) nationally and then by province, with the mean vote share by constituency in each region along with the 90% confidence interval around the mean. INSERT FIGURE 6 ABOUT HERE. PPP losses are attenuated dramatically nationally and in Punjab (where they lost the most relative to 2008) in flood-affected areas. On average the PPP vote share dropped 17.6 percentage 32 points of vote share nationally from 2008 to 2013, but they lost 21.1 percentage points in constituencies with nobody affected by the floods and only 13.9 percentage points in flood-affected constituencies, a difference significant at the .005 level in a two-tailed t-test for difference in means. For the PML-N, the main opposition party, the gains are larger in flood affected places, particularly in KPK and Sindh. Those gains come at the expense of ethnic and religious parties in those places as the PPP lost a bit less in flood-affected areas in KPK and Sindh. Neither party saw any significant difference across flood-affected regions in the provinces they have long dominated. In Sindh, where the PPP has its stronghold, the party lost fewer votes in flood-affected places, but the difference is marginal. In Punjab, which had been run by the PML-N for many years, the party gained very slightly in flood-affected places, but again, the difference is small. As Table 10 shows, these results are robust to include the same geographic controls as in the other regressions plus a province fixed-effect to account for the parties’ differential organizational capacities across provinces. While the results are not uniformly strong, they are inconsistent with blind retrospection (Achen and Bartels, 2004) and provide modest evidence that the PPP suffered less in flood-affected areas where they did not have an entrenched advantage and those their performance could make a difference (i.e. Punjab). INSERT TABLE 10 HERE Critically, the PML-N campaigned in 2013 as the party of effective governance. Given that, the large changes in their favor in flood-affected places are consistent with the possibility that the floods shifted political behavior by dramatically reinforcing the importance of government. In flood-affected areas, voters gave the incumbent some credit for its good relief efforts (as we noted, the number killed was remarkably low given the extent of the devastation), but also moved relatively more strongly towards the party which campaigned on effective governance and policy execution. Flood exposure substantially decreased the vote shares of small parties that make ethnic, sectarian, and locality-specific appeals. In the face of such obvious evidence that government can competently address crises, people seem to have turned away from patronage politics in favor of more programmatic parties. 33 Support for Militant Organizations: Endorsement Experiment Contrary to the worries of many in the media, we find no evidence that support for militancy is higher among those affected by the floods. Although the impact of flooding increased people’s abstract support for violent political action, that did not appear to translate into a taste for nonstate actors. Across the same seven objective and subjective measures of flood impacts support for militant groups (as measured by the endorsement experiment) is consistently lower among the floodaffected. Table 11 reports β3 from equation (3) across the core flood measures when we average across militant groups (Panel A), and for each of the militant groups separately: the sectarian group Sipah-e-Sahaba Pakistan (SSP) (Panel B), the Pakistan Taliban (Panel C), which claimed to be administering flood relief in some parts of KPK, and the Afghan Taliban (Panel D) which rarely, if ever, conduct violent activities in Pakistan. β3 is negative in all regressions and depending on the measure of flood effects, we reject the one-tailed null that the floods had a positive impact on support for militants on average at the 95% percent level for most objective measures and at the 80% level on average for the subjective measures. INSERT TABLE 11 HERE Nor did militant service provision in flood-affected areas help them generate support. We collected data on all locations where militants were providing relief and which organizations were doing so using a Lexis-Nexis search of all flood coverage between July 1 and October 1, 2010. We augmented these results by reviewing electronically-available Pakistani news sources.30 Despite the international media coverage that seemed to suggest that militants were at the forefront of aid delivery, we found fewer than two dozen sites of militant relief camps. Including a dichotomous variable for whether a tehsil had militant relief camp in the regressions from table 11—either interacted with the endorsement experiment or on its own—yields no evidence in the direction of greater support for militant groups if they had a relief camp. The negative impact of flooding on support for militant organizations is actually substantively larger in districts that had observed militant relief camps and is more than twice as strong statistically. 30 The newspapers included in our search are: Pakistan Express Tribune, The Dawn, The News, and The Nation. 34 5.4 Ruling Out Patronage So far we have seen that citizens in flood-affected areas have more aggressive attitudes about how to petition for services, know more about politics, and turnout to vote at higher rates. An important possibility to rule out is that these differences merely reflect the fact that patronage goods were dispensed under the guise of flood relief. This is particularly important for assessing the results on turnout and incumbent vote share. The data provide several reasons to think the results are not driven by patronage. First, as Table 12 shows, people were not discernibly happier with the government response in floodaffected areas as compared to non-affected ones. We asked respondents whether they thought the government did a good job of dealing with the floods (on a 4-point scale from very bad job to very good job)) and whether they thought their town was given better relief than other towns (on a 3-point scale of better, the same, and worse). Neither indicator is consistently correlated with flood exposure after adding our standard controls (if anything those in the hardest hit areas think the government did a worse job), a fact that is not consistent with people voting at higher rates to reward politicians for providing differential levels of patronage goods. INSERT TABLE 12 HERE Second, the flood effect on turnout is weakest in Sindh, where the PPP’s ability to distribute patronage was strongest as it controlled both the national and provincial governments. Third, the relative gain for the PPP in flood-affected areas vs. other areas of Sindh is very weak. In Sindh, PPP actually loses votes in flood-affected constituencies relative to PML-N. Fourth, the impact of the flood on political knowledge is strongly positive for the objective measures of those impacts and weakly so for subjective ones, which is consistent with citizens living in flood-affected places becoming more engaged but is not a prediction of the patronage argument. Finally, if the results were driven by patronage we might expect that the probability that the incumbent party in 2008 lost in 2013 would be lower in flood-affected places where the Member of the National Assembly in power had chances to use his/her development funds. That’s not the case, as there is no statistically detectable difference between reelection probabilities across levels of flood exposure in NA or PA elections and the turnover probability is generally a bit higher in flood-affected places. 35 6 Discussion In assessing how the devastating 2010-11 floods affected political attitudes and behavior among Pakistani citizens, we found five empirical regularities. First, citizens exposed to the 2010-11 floods were more likely to think violent protests would be effective in achieving government responsiveness and more approving of this method than signing and presenting politicians with a petition. Second, flood-affected citizens are more knowledgeable about politics. Third, flood victims did not become more supportive of non-state militant groups, if anything they turned against them. Fourth, turnout increased more in flood-affected constituencies from 2008 to 2013 than elsewhere. Fifth, citizens living in flood affected areas in the country’s largest province appear to have given the previous incumbent some credit for its performance in responding to the floods, while citizens living in flood-affected constituencies throughout the country turned away from parties making highly particularistic appeals and towards the party that ran on a more programmatic platform. This final section provides a possible theoretical interpretation of these empirical regularities, discusses policy implications, and points towards avenues for future research. 6.1 Theoretical Implications Our results provide an important note of caution for research using natural disasters to study economic mechanism that might explain how states make the transition from autocracy to democracy and then on to functioning programmatic politics. In Pakistan a major disaster that created a transient negative economic shock also led to a range of changes in citizens’ political attitudes and behavior. A broad range of formal and informal theories suggest that informed and civically engaged citizens are able to enforce better governance by providing politicians with incentives to become more responsive and focus on public goods provision rather than relying on patronage or particularistic and ethnic appeals to retain office. Researchers should therefore be careful of assuming a mono-causal, economic mechanism through which similar shocks affect governance. Disasters may instead lead to a range of attitudinal and behavioral changes among citizens that alter the costs and benefits politicians face from policy choices. We believe the observed empirical patterns are consistent with the following interpretation. Victims of the 2010-11 floods in Pakistan experienced a sudden and unexpected need for disaster 36 relief. Due to the massive scale of the disaster, the necessary coordination for managing international aid and equipment for getting it to people could only be provided by the government. This event thus had unusual power for making citizens aware of how important it is to have a responsive government providing basic services. This in turn increased their willingness to aggressively demand government services, but did not push people to abandon democratic institutions in support of non-state actors. To the contrary, those hit hardest became more politically engaged, as captured by increased level of electoral turnout in the 2013 elections and their increased accumulation of political knowledge. The exact mechanism through which flood exposure caused this change in political attitudes, however, remains open. We see at least two plausible mechanisms. The first is a straightforward informational story. Through their experience, flood victims may have gained new information on the proper role of government and its alternatives, which affected their beliefs about the importance of good governance. For example, citizens hit by the flood experienced first hand how crucial the effective provision of basic government services, such as disaster relief in form of shelter, sanitation, food, and access to clean drinking, can be and learn that there is little alternative to government action when it comes to providing theses services rapidly and at a large scale. This experience and insight may have changed their attitudes towards government negligence and incompetence, causing them to become more politically involved but also more supportive of unconventional forms of demanding government action. Alternatively, the mechanism linking flood exposure to the observed changes in political attitudes and behavior may lay in deep shifts of preferences and values. A considerable body of psychological research finds that reports of “post-traumatic growth” experiences consistently outnumber reports of psychiatric disorders (Tedeschi and Calhoun, 2004). Among other domains of personal growth after traumatic experiences, this line of research finds that victims experience a changed sense of priorities, a greater sense of personal strength, and recognition of new possibilities or paths for one’s life (e.g., Nolen-Hoeksema and Davis, 2002; Laufer and Solomon, 2006). Several recent papers in conflict research have found that exposure to violence is robustly linked to greater political engagement and a higher willingness to contribute to a collective good. Bellows and Miguel (2009), for example, observe that individuals in Sierra Leone whose households experienced more intense war violence are more likely to attend community meetings, more likely to 37 join local political and community groups, and more likely to vote. Using data from child soldiers in Northern Uganda, Blattman (2009) shows that past experience of violence resulted in greater political participation in the post-war period. Drawing on experimental data from 35 randomly selected communities in Burundi, Voors et al. (2012) find that individuals that have been exposed to greater levels of violence display more altruistic behavior towards their neighbors, are more risk seeking, and have higher economic discount rates. Finally, Gilligan, Pasquale and Samii (2011) find that members of communities with greater exposure to violence during Nepal’s ten-year civil war exhibit significantly greater levels of social capital, measured by the subjects willingness to invest in trust-based transactions and contribute to a collective good. Granted, victimization in civil war is qualitatively different from being a victim of flooding. Yet, fearing for your own life and the lives of loved ones in the wake of flash floods may nevertheless qualify as a traumatic event that is sufficiently strong to unleash the described psychological process resulting in the change of preferences, values, and ultimately political attitudes. Through which mechanism do changes in political attitudes affect political behavior? We believe that “expressive” theories of participation offer a possible explanation. These theories argue that individuals engage in otherwise too costly political actions (e.g., protesting or voting) because they value the act of political expression itself. Citizens, for example, turn out to vote not because of purely materialistic incentives, but because of a “sense of civic duty” (e.g., Riker and Ordeshook, 1968) or because of the inherent value they place on the act of voting itself (e.g., Dhillon and Peralta, 2002; Feddersen, 2004). The origin of such a “ sense of civic duty” or inherent value of political participation and the reason why it varies across citizens and time is not yet well understood. The informational and psychological mechanisms above may help fill this gap. Traumatic events such as the massive 2010-11 floods in Pakistan may contribute to changes in victims’ political attitudes through either an informational process or a reordering of personal goals and priorities. These in turn may increases their “sense of civic duty” and thus their willingness to vote. 6.2 Policy Implications Our findings are good news for policy makers worried that natural disasters in weakly institutionalized countries will weaken fragile democratic institutions. As the Pakistani example shows, this need not be the case. Exposure to natural disasters might actually highlight the necessity of gov38 ernmental services and strengthen citizen’s willingness to demand government responsiveness and increase their engagement in democratic process. A key avenue for future research is the extent to which these salutary effects are conditioned on an effective government response in the aftermath of the disaster. At a minimum, these results highlight the importance of making sure governments can respond effectively to disasters. Beyond the humanitarian imperative, supporting such a response may enhance prospects for long-run improvements in governance. There are, however, important limitations to our research.The political attitudes (i.e., way to interact with the government, support for militants) measured in the survey and the political behaviors studied (i.e., electoral turnout and major party vote share) took place in an important, but very specific context. In particular, Pakistani politics are very poorly institutionalized relative to many polities, with politicians historically switching parties to deliver their vote banks to whomever offers them the best patronage opportunities. Though similar conditions are found in other countries (e.g., parts of India) the specificity of the Pakistani context should be kept in mind when generalizing the findings to political attitudes and behavior more broadly. Our results may not apply to other countries with a different institutional structures, different types of militant groups, and different levels of international support in the aftermath of a natural disaster. 6.3 Future Research Still, our analysis highlights several avenues for future research. For instance, it is important to uncover the causal mechanism underlying the impact of flood exposure on political attitudes and behavior. Does a natural disaster alter victims’ preferences and/or political values or does it simply provide useful information and a concrete experience that teaches victims the value of democracy and government responsiveness? Distinguishing these two mechanisms is challenging as changes to preferences and values are notoriously hard to measure. Another avenue is to study how long the observed beneficial effects on political participation persist. Will the effect sustain over time, suggesting that the flood caused an enduring change in political participation? The fact that we were able to detect the effect three years after the floods provides some evidence that the effect is quiet persistent. Finally, we need to extend this analysis to further parse the mechanisms behind the effects identified above. In particular, the National Disaster Management Agency of Pakistan collected 39 remarkably fine-grained data on what kinds of aid were delivered, where, and by whom. Future research can assess how these results vary by average levels of aid provided. 40 Figures Figure 1: Standardized Impact of Floods in Pakistan 1975 – 2012 41 Figure 2: Balance of Covariates for the Vignette Experiment 42 Figure 3: Balance of Covariates for the Endorsement Experiment 43 Figure 4: Composite Maximal Flood Extent in 2010 and 2011 and Surveyed Tehsils 44 Figure 5: Variance in Flood Impacts between National and Provincial Assembly Constituencies 45 46 Figure 6: Major Party Vote Shares in Constituencies by Flood Exposure Tables Variables % Area Flooded 2010 & 2011 % Population Exposed 2010 & 2011 Population Exposed > Median == 1 Population Exposed > 90th Percentile == 1 Flood Exposure Affected == 1 Very Bad | Extremely Bad == 1 Distance to River Neighboring River == 1 Std. Dev. of Elevation Mean of Elevation Male Head of Household Age Read Math Education Sunni Political Knowledge (PCA) Political Knowledge (Additive) Satisfaction Government Relief Effort Government Relief Comparison Other Towns % Area Flooded 2010 & 2011 Area Exposed > Median == 1 Area Exposed > 90th Percentile == 1 % Population Exposed 2010 & 2011 Population Exposed <= Median == 1 Population Exposed > Median == 1 Population Exposed > 90th Percentile == 1 Affected (NDMA) == 1 % Population Exposed 2012 Distance to River Neighboring River == 1 Std. Dev. of Elevation Mean of Elevation Turnout Diff. 2013-2008 Diff. in Turnout Diff. (2013-2008)-(2008-2002) PPP Vote Share Diff. 2013-2008 PML-N Vote Share Diff. 2013-2008 % Area Flooded 2010 & 2011 Area Exposed > Median == 1 Area Exposed > 90th Percentile == 1 % Population Exposed 2010 & 2011 Population Exposed > Median == 1 Population Exposed > 90th Percentile == 1 Affected (NDMA) == 1 % Population Exposed 2012 Distance to River Neighboring River == 1 Std. Dev. of Elevation Mean of Elevation Turnout Diff. 2013-2008 Diff. in Turnout Diff. (2013-2008)-(2008-2002) Unit percent percent dummy dummy 4 pt. scale [0,1] dummy dummy 100 kilometers dummy 1,000 meters 1,000 meters dummy dummy 100 years dummy dummy 6 pt. scale [0,1] dummy index index [0,1] 4 pt. scale [1,4] 3 pt. scale [1,3] percent dummy dummy percent dummy dummy dummy dummy percent 100 kilometers dummy 1,000 meters 1,000 meters [-1,1] [-1,1] percent percent percent dummy dummy percent dummy dummy dummy percent 100 kilometers dummy 1,000 meters 1,000 meters [-1,1] [-1,1] Level Tehsil Tehsil Tehsil Tehsil Individual Individual Individual Tehsil Tehsil Tehsil Tehsil Individual Individual Individual Individual Individual Individual Individual Individual Individual Individual Individual NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency NA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency PA-Constituency N 12994 12994 12994 12994 12994 12994 12994 12994 12994 12994 12994 12994 12968 12990 12931 12367 12889 12923 12994 12994 12240 11671 249 249 249 249 249 249 249 249 249 249 249 249 249 249 249 249 249 569 569 569 569 569 569 569 569 569 569 569 569 569 569 Median 0 0 0 0 0.250 0 0 0.331 0 0.029 0.191 1 0 0.340 1 1 0.167 1 2.120 0.700 2 2 0 0 0 0 0 0 0 1 0 0.260 1 0.007 0.179 0.114 0.083 -0.158 0.051 0 0 0 0 0 0 0 0 0.269 0 0.006 0.179 0.112 0.077 Mean 0.083 0.059 0.222 0.047 0.385 0.268 0.181 0.899 0.469 0.128 0.540 0.515 0.373 0.350 0.545 0.776 0.275 0.930 2.024 0.673 2.417 1.838 0.082 0.253 0.052 0.065 0.233 0.249 0.052 0.510 0.012 0.482 0.522 0.093 0.351 0.113 0.086 -0.165 0.11 0.086 0.220 0.042 0.067 0.206 0.042 0.464 0.013 0.579 0.373 0.084 0.388 0.103 0.072 Std. Dev. 0.157 0.136 0.416 0.211 0.248 0.443 0.385 1.242 0.499 0.195 0.724 0.500 0.484 0.119 0.498 0.417 0.281 0.256 0.741 0.227 0.863 0.644 0.150 0.436 0.223 0.127 0.424 0.433 0.223 0.501 0.052 0.715 0.501 0.198 0.575 0.079 0.141 0.166 0.194 0.167 0.414 0.201 0.146 0.405 0.201 0.499 0.062 0.893 0.484 0.175 0.598 0.094 0.150 Table 1: Summary Statistics of the Covariates Across Datasets 47 Min 0 0 0 0 0.25 0 0 0.005 0 0.002 0.005 0 0 0.18 0 0 0 0 0 0 1 1 0 0 0 0 0 0 0 0 0 0.016 0 0 0.004 -0.114 -0.371 -0.59 -0.489 0 0 0 0 0 0 0 0 0.001 0 0 0.002 -0.416 -0.544 Max 0.928 0.897 1 1 1 1 1 6.856 1 1.021 4.247 1 1 0.85 1 1 1 1 3.006 1 4 3 0.79 1 1 0.61 1 1 1 1 0.489 5.517 1 1.097 3.922 0.372 0.638 0.388 0.669 0.912 1 1 1 1 1 1 0.7 6.353 1 1.059 4.243 0.506 0.822 (1) (2) (3) (4) Independent % Area % Population Pop. Exposed > Pop. Exposed > Variable: Flooded Exposed Median 90th Percentile Panel A: Effectiveness of Junaid's/Mahir's Actions (mean = 0.65, sd in non-violent = 0.30, sd in violent = 0.38) β1: Violent Vignette β2: Flood Treatment β3: Violent * Flood -0.215*** (0.018) 0.208** (0.105) 0.198** (0.086) -0.216*** (0.018) 0.058 (0.107) 0.282*** (0.096) -0.220*** (0.019) 0.040 (0.041) 0.089*** (0.033) -0.204*** (0.016) -0.040 (0.047) 0.118** (0.058) 48 R-squared 0.237 0.235 0.235 0.232 Observations 11963 11963 11963 11963 Clusters 1094 1094 1094 1094 Panel B: Approval of Junaid's/Mahir's Actions (mean = 0.62, sd in non-violent = 0.31, sd in violent = 0.39) β1: Violent Vignette β2: Flood Treatment β3: Violent * Flood -0.229*** (0.019) 0.076 (0.116) 0.213** (0.088) -0.230*** (0.018) -0.069 (0.114) 0.325*** (0.097) -0.232*** (0.019) 0.032 (0.041) 0.089*** (0.034) -0.218*** (0.017) -0.121** (0.049) 0.172*** (0.055) (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad -0.248*** (0.026) 0.066* (0.036) 0.129*** (0.049) -0.221*** (0.018) 0.010 (0.022) 0.083*** (0.030) -0.209*** (0.017) 0.050** (0.021) 0.058* (0.031) 0.237 11963 1094 0.236 11963 1094 0.236 11963 1094 -0.274*** (0.027) -0.007 (0.039) 0.165*** (0.052) -0.240*** (0.019) -0.039 (0.023) 0.112*** (0.032) -0.225*** (0.018) 0.017 (0.023) 0.081** (0.032) R-squared 0.252 0.253 0.253 0.251 0.253 0.253 0.252 Observations 11963 11963 11963 11963 11963 11963 11963 Clusters 1094 1094 1094 1094 1094 1094 1094 Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regression include; district fixed effects; geographic controls at the tehsil level, including distance to major river, dummy for tehsils boardering a major river, std. dev. of the tehsil's elevation, and mean tehsil elevation; and demographic controls including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Table 2: Impact of Flooding on Approval and Perceived Efficacy of Violent Protest (1) (2) Independent Self-Reported Self-Reported Variables: Flood Exposure Affected Panel A: Effectiveness of Junaid's/Mahir's Actions (mean = 0.65) β1: Violent Vignette β2: Flood Treatment β3: Violent * Flood -0.256*** (0.027) 0.068** (0.034) 0.138*** (0.046) -0.224*** (0.019) 0.019 (0.021) 0.080*** (0.029) R-squared 0.306 0.305 Observations 11963 11963 Clusters 1094 1094 Panel B: Approval of Junaid's/Mahir's Actions (mean = 0.62) β1: Violent Vignette β2: Flood Treatment β3: Violent * Flood -0.283*** (0.028) 0.004 (0.038) 0.182*** (0.050) -0.241*** (0.020) -0.025 (0.023) 0.107*** (0.031) (3) Self-Reported Very | Extremely Bad -0.215*** (0.018) 0.043** (0.020) 0.063** (0.029) 0.305 11963 1094 -0.230*** (0.019) 0.016 (0.022) 0.093*** (0.031) R-squared 0.322 0.322 0.322 Observations 11963 11963 11963 Clusters 1094 1094 1094 Notes: Exposure measures calculated at the individual level. All regressions include; tehsil fixed effects and demographic controls, including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Table 3: Impact of Flooding on Perceived Efficacy and Approval of Violent Protest with Tehsil Fixed Effects 49 (1) (2) Independent % Area % Population Variables: Flooded Exposed Panel A: Effectiveness of Junaid's/Mahir's Actions (mean = 0.66) β1: Violent Vignette β2: Flood Treatment β3: Violent * Flood -0.203*** (0.027) -0.027 (0.111) 0.237** (0.094) -0.204*** (0.024) -0.186* (0.099) 0.409*** (0.093) 50 R-squared 0.227 0.230 Observations 5685 5685 Clusters 513 513 Panel B: Approval of Junaid's/Mahir's Actions (mean = 0.62) β1: Violent Vignette β2: Flood Treatment β3: Violent * Flood -0.230*** (0.028) -0.081 (0.130) 0.258** (0.103) -0.230*** (0.025) -0.224** (0.109) 0.434*** (0.098) (3) Pop. Exposed > Median (4) Pop. Exposed > 90th Percentile (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad -0.214*** (0.026) -0.087* (0.046) 0.152*** (0.040) -0.183*** (0.022) -0.109*** (0.035) 0.171*** (0.055) -0.253*** (0.034) -0.035 (0.042) 0.218*** (0.056) -0.201*** (0.024) -0.038 (0.028) 0.124*** (0.038) -0.193*** (0.023) -0.016 (0.025) 0.125*** (0.035) 0.232 5685 513 0.226 5685 513 0.230 5685 513 0.229 5685 513 0.229 5685 513 -0.241*** (0.028) -0.094** (0.044) 0.163*** (0.043) -0.209*** (0.023) -0.171*** (0.046) 0.207*** (0.057) -0.283*** (0.036) -0.120** (0.051) 0.235*** (0.064) -0.229*** (0.025) -0.080** (0.031) 0.145*** (0.041) -0.216*** (0.024) -0.060** (0.030) 0.124*** (0.040) R-squared 0.253 0.257 0.259 0.255 0.255 0.256 0.253 Observations 5685 5685 5685 5685 5685 5685 5685 Clusters 513 513 513 513 513 513 513 Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regressions include: district fixed effects; geographic controls at the tehsil level, including distance to major river, std. dev. of the tehsil's elevation, and mean tehsil elevation; and demographic controls including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Table 4: Impact of Flooding on Perceived Efficacy and Approval of Violent Protest in Tehsils Bordering Major Rivers Comparison of Main Effect Controls in the Controls in the to Bias Accounted for by Restricted Set Full Set Panel A: Effectiveness of Junaid's/Mahir's Actions Controling for individual District FE and demographics District FE Demographics Controling for demographics and tehsil geography Controling for all common district-specfic factors % Area Flooded % Population Exposed Pop. Exposed > Median Independent Variables Pop. Exposed > 90th Percentile Self-Reported Flood Exposure Self-Reported Affected Self-Reported Very | Extremely Bad -23.603 -52.190 -14.622 30.514 -77.240 -59.049 -27.179 District FE Full Set of Controls as in Table 2 -15.523 -26.814 -9.939 59.602 -32.063 -32.737 -18.537 Geographic and Demographics Full Set of Controls as in Table 2 2.773 5.376 -15.660 5.411 2.095 2.356 1.678 51 Panel B: Approval of Junaid's/Mahir's Actions Controling for individual demographics District FE District FE and Demographics -20.713 -50.145 -12.405 40.432 -81.275 -59.395 -32.242 Controling for demographics and tehsil geography District FE Full Set of Controls as in Table 2 -14.044 -29.854 -8.984 71.124 -37.358 -37.939 -22.221 Controling for all common district-specfic factors Geographic and Demographics Full Set of Controls as in Table 2 2.439 5.153 6.610 5.808 2.743 3.696 2.313 Notes: Each Cell in the table reports ratios based on the coefficient of β3 (i.e., Violent Vignette * Flood) from two individual-level regressions. In one, the covariates include the "restricted set" of control variables; call this coefficient βR. In the other, the covariates include the "full set" of controls; call this coefficient βF. In both regressions, the sample sizes are the same. The reported ratio is calculated as: βF/(βR-βF). Geographic controls at the tehsil level include distance to major river, dummy for tehsils boardering a major river, std. dev. of the tehsil's elevation, and mean tehsil elevation. Demographic controls include gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Table 5: Using Selection on Observables to Assess the Bias from Unobservables (1) (2) (3) (4) Independent % Area % Population Pop. Exposed > Pop. Exposed > Variable: Flooded Exposed Median 90th Percentile Panel A: Index of Political Knowledge (Principal Component Analysis) (mean = 2.024, sd = 0.741) Flood Treatment 0.168 (0.122) 0.453*** (0.132) 0.077 (0.056) R-squared 0.375 0.376 0.375 Observations 12178 12178 12178 Clusters 1097 1097 1097 Panel B: Index of Political Knowledge (Additive) (mean = 0.673, sd = 0.227) (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad 0.213*** (0.058) 0.149*** (0.052) 0.101*** (0.030) 0.062** (0.029) 0.376 12178 1097 0.376 12178 1097 0.376 12178 1097 0.375 12178 1097 52 Flood Treatment 0.047 (0.036) 0.136*** (0.039) 0.020 (0.016) 0.063*** (0.018) 0.038** (0.016) 0.025*** (0.009) 0.016* (0.009) R-squared Observations Clusters 0.380 12178 1097 0.381 12178 1097 0.380 12178 1097 0.381 12178 1097 0.381 12178 1097 0.381 12178 1097 0.380 12178 1097 Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regressions include: district fixed effects; geographic controls at the tehsil level including distance to major river, dummy for tehsils boardering a major river, std. dev. of the tehsil's elevation, and mean tehsil elevation; and demographic controls including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education. and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Table 6: Impact of Flooding on Political Knowledge (1) (2) (3) (4) (5) (6) Independent % Area Area Exposed > Area Exposed > % Population Pop. Exposed > Pop. Exposed > Variables: Flooded Median 90th Percentile Exposed Median 90th Percentile Panel A: Turnout Change (2013 - 2008) with Division Fixed Effects (mean = 0.11, sd = 0.08) Flood Treatment 0.109* (0.056) 0.034** (0.016) 0.034 (0.023) R-squared 0.306 0.308 0.299 Observations 246 246 246 Clusters 90 90 90 Panel B: First Differences ((2013-2008)-(2008-2002)) (mean = 0.09, sd = 0.14) Flood Treatment 0.234*** (0.072) 0.074*** (0.025) 0.089*** (0.033) 0.162** (0.070) 0.016 (0.018) 0.054* (0.028) 0.313 246 90 0.294 246 90 0.305 246 90 0.308*** (0.094) 0.055** (0.026) 0.099** (0.041) 0.060 246 90 0.056 246 90 0.032 (0.031) 0.084* (0.046) R-squared 0.079 0.077 0.056 0.085 Observations 246 246 246 246 Clusters 90 90 90 90 Panel C: First Differences ((2013-2008)-(2008-2002)) with Division Fixed Effects Flood Treatment 0.249** (0.103) 0.060* (0.030) 0.079** (0.039) 0.314** (0.127) R-squared 0.279 0.271 0.267 0.280 0.258 0.266 Observations 246 246 246 246 246 246 Clusters 90 90 90 90 90 90 Notes: Exposure measures calculated at the constituency level. All regressions include geographic controls at the constituency level including distance to major river, dummy for constituencies boardering a major river, std. dev. of the constituency's elevation, and mean constituency elevation, as well as the proportion of constituency population exposed to the 2012 floods. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the district level. Table 7: Impact of Flooding on Turnout in the 2013 Pakistani National Assembly Elections 53 (1) (2) (3) (4) (5) (6) Independent % Area Area Exposed > Area Exposed > % Population Pop. Exposed > Pop. Exposed > Variables: Flooded Median 90th Percentile Exposed Median 90th Percentile Panel A: Turnout Change (2013 - 2008) with Division Fixed Effects (mean = 0.10, sd = 0.09) Flood Treatment 0.112*** (0.035) 0.031*** (0.011) 0.034** (0.016) R-squared 0.311 0.305 0.300 Observations 556 556 556 Clusters 109 109 109 Panel B: First Differences ((2013-2008)-(2008-2002)) (mean = 0.07, sd = 0.15) Flood Treatment 0.237*** (0.068) 0.084*** (0.025) 0.092*** (0.035) 0.110** (0.046) 0.028** (0.012) 0.022 (0.019) 0.308 556 109 0.030 556 109 0.298 556 109 0.246** (0.098) 0.077*** (0.024) 0.065* (0.039) 0.098 556 109 0.073 556 109 0.063*** (0.022) 0.038 (0.036) R-squared 0.110 0.105 0.080 0.102 Observations 556 556 556 556 Clusters 109 109 109 109 Panel C: First Differences ((2013-2008)-(2008-2002)) with Division Fixed Effects Flood Treatment 0.222*** (0.062) 0.065*** (0.022) 0.067** (0.032) 0.196** (0.094) R-squared 0.277 0.269 0.260 0.268 0.267 0.256 Observations 556 556 556 556 556 556 Clusters 91 91 91 91 91 91 Notes: Exposure measures calculated at the constituency level. All regressions include geographic controls at the constituency level including distance to major river, dummy for constituencies boardering a major river, std. dev. of the constituency's elevation, and mean constituency elevation, as well as the proportion of constituency population exposed to the 2012 floods. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the district level. Table 8: Impact of Flooding on Turnout in the 2013 Pakistani Provincial Assembly Elections 54 (1) (2) (3) (4) (5) (6) Independent % Area Area Exposed > Area Exposed > % Population Pop. Exposed > Pop. Exposed > Variables: Flooded Median 90th Percentile Exposed Median 90th Percentile Panel A: Turnout Change (2013 - 2008) Including Migration Estimate (mean = 0.11, sd = 0.08) Flood Treatment 0.069 (0.060) 0.015 (0.016) 0.026 (0.027) 0.175** (0.082) 0.024 (0.021) 0.052* (0.027) Migrated 0.186 (0.201) 0.197 (0.202) 0.170 (0.205) 0.199 (0.199) 0.186 (0.200) 0.169 (0.206) R-squared 0.454 0.452 0.453 0.467 0.454 Observations 158 158 158 158 158 Clusters 52 52 52 52 52 Panel B: Turnout Change (2013 - 2008) in NA-Constituencies Without Migration (mean = 0.12, sd = 0.07) Flood Treatment 0.079 (0.053) 0.029** (0.014) 0.024 (0.023) 0.134** (0.065) 0.012 (0.017) R-squared 0.326 0.332 0.320 0.338 0.317 Observations 157 157 157 157 157 Clusters 69 69 69 69 69 Panel C: Turnout Change (2013 - 2008) in PA-Constituencies Without Migration (mean = 0.12, sd = 0.07) Flood Treatment 0.089*** (0.033) 0.024** (0.011) 0.030* (0.016) 0.090** (0.044) 0.022* (0.011) 0.459 158 52 0.053* (0.029) 0.337 157 69 0.018 (0.018) R-squared 0.314 0.307 0.305 0.312 0.306 0.302 Observations 378 378 378 378 378 378 Clusters 87 87 87 87 87 87 Notes: Exposure measures calculated at the constituency level. All regressions include division fixed effects and geographic controls at the constituency level including distance to major river, dummy for constituencies boardering a major river, std. dev. of the constituency's elevation, and mean constituency elevation, as well as the proportion of constituency population exposed to the 2012 floods. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the district level. Table 9: Evidence That Turnout Increase Is Not Due to a Composition Effect 55 National (1) (2) Political Party: PPP PML-N Panel A: Change in Vote Share (2013 - 2008) Geographic Extent: Affected (NDMA) 0.062** (0.030) 0.037 (0.037) Balochistan (3) (4) PPP PML-N 0.033 (0.092) 0.003 (0.045) R-squared 0.063 0.107 0.015 0.001 Observations 249 249 13 13 Clusters 91 91 11 11 Panel B: Change in Vote Share (2013 - 2008) with Control Variables Affected (NDMA) 0.054 (0.035) 0.017 (0.041) 0.003 (0.107) -0.053 (0.115) KPK Punjab Sindh 56 (5) PPP (6) PML-N (7) PPP (8) PML-N (9) PPP (10) PML-N 0.016 (0.094) 0.059* (0.031) 0.089** (0.038) 0.033 (0.031) 0.012 (0.038) 0.063** (0.023) 0.002 34 22 0.031 34 22 0.062 143 36 0.005 143 36 0.001 57 21 0.055 57 21 -0.028 (0.076) 0.071 (0.046) 0.096** (0.042) -0.017 (0.053) -0.012 (0.128) 0.043** (0.020) 0.128 143 36 0.059 57 21 0.265 57 21 R-squared 0.087 0.124 0.456 0.348 0.162 0.235 0.086 Observations 249 249 13 13 34 34 143 Clusters 91 91 11 11 22 22 36 Panel C: Change in Vote Share (2013 - 2008) with Control Variables (Baseline Categorie: Unaffected Constituencies) Population Exposed >0 and ≤ Median 0.039 (0.038) 0.022 (0.041) -0.003 (0.103) -0.051 (0.110) 0.006 (0.061) 0.124** (0.043) 0.068 (0.047) -0.020 (0.055) -0.039 (0.148) 0.037 (0.026) Population Exposed > Median 0.087* (0.044) 0.030 (0.044) 0.117 (0.123) -0.143 (0.134) -0.081 (0.088) 0.153** (0.072) 0.153* (0.079) -0.011 (0.062) 0.090* (0.051) 0.024 (0.030) R-squared 0.095 0.137 0.479 0.393 0.205 0.240 0.103 0.112 0.117 0.266 Observations 249 249 13 13 34 34 143 143 57 57 Clusters 91 91 11 11 22 22 36 36 21 21 Notes: Exposure measures calculated at the constituency level. Regressions in Panel B and C include geographic controls at the constituency level, including distance to major river, dummy for constituencies boardering a major river, std. dev. of the constituency's elevation, and mean constituency elevation, as well as the proportion of constituency population exposed to the 2012 floods. National-level regressions (Models 1 and 2) also include province fixed effects. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). All standard errors are clustered at the district level. Table 10: Impact of Flooding on the Differences in the PPP’s and PML-N’s Vote Shares between 2013 and 2008 (1) (2) (3) Independent % Area % Population Pop. Exposed > Variables: Flooded Exposed Median Panel A: All Militant Groups (mean policy prefernce in control group = 0.62, sd = 0.26) (4) Pop. Exposed > 90th Percentile (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad β3: Militant * Flood -0.144** (0.068) -0.133* (0.072) -0.062** (0.031) -0.063 (0.045) -0.043 (0.043) -0.036 (0.030) -0.019 (0.026) p-value for H0: β3>0 0.02 0.03 0.02 0.08 0.16 0.12 0.26 0.308 8443 828 0.310 8443 828 0.306 8443 828 0.307 8443 828 0.306 8443 828 R-squared 0.308 0.308 Observations 8443 8443 Clusters 828 828 Panel B: SSP (mean policy prefernce in control group = 0.63, sd = 0.25) 57 β3: Militant * Flood -0.142 (0.088) -0.143 (0.088) -0.067* (0.040) -0.068 (0.052) -0.039 (0.049) -0.041 (0.032) -0.015 (0.030) p-value for H0: β3>0 0.05 0.05 0.05 0.09 0.21 0.10 0.31 R-squared 0.304 0.306 0.304 Observations 4231 4231 4231 Clusters 420 420 420 Panel C: Pakistan Taliban (mean policy prefernce in control group = 0.63, sd = 0.25) 0.306 4231 420 0.301 4231 420 0.302 4231 420 0.301 4231 420 β3: Militant * Flood -0.209** (0.105) -0.289*** (0.109) -0.078* (0.043) -0.153** (0.068) -0.058 (0.062) -0.061 (0.041) -0.014 (0.037) p-value for H0: β3>0 0.02 0.00 0.03 0.01 0.17 0.07 0.35 R-squared 0.303 0.304 0.303 Observations 4250 4250 4250 Clusters 423 423 423 Panel D: Afghan Taliban (mean policy prefernce in control group = 0.62, sd = 0.26) 0.303 4250 423 0.300 4250 423 0.302 4250 423 0.300 4250 423 β3: Militant * Flood -0.148* (0.079) -0.115 (0.081) -0.066 (0.041) -0.040 (0.046) -0.049 (0.051) -0.025 (0.034) -0.025 (0.031) p-value for H0: β3>0 0.03 0.08 0.06 0.20 0.17 0.24 0.21 R-squared 0.390 0.391 0.390 0.395 0.388 0.389 0.388 Observations 4228 4228 4228 4228 4228 4228 4228 Clusters 425 425 425 425 425 425 425 Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regressions include: district fixed effects; geographic controls at the tehsil level including distance to major river, dummy for tehsils boardering a major river, std. dev. of the tehsil's elevation, and mean tehsil elevation; and demographic controls including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Table 11: Impact of Flooding on the Support for Militant Groups (1) (2) Independent % Area % Population Variable: Flooded Exposed Panel A: Did Government Do a Good Job? (mean = 2.024, sd = 0.741) Flood Treatment 0.235 (0.190) -0.037 (0.171) 58 R-squared 0.207 0.206 Observations 10848 10848 Clusters 1047 1047 Panel B: Did Other Town Get Better Relief? (mean = 0.673, sd = 0.227) Flood Treatment 0.006 (0.148) -0.166 (0.151) (3) Pop. Exposed > Median (4) Pop. Exposed > 90th Percentile (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad 0.108 (0.081) -0.195** (0.084) -0.032 (0.070) -0.027 (0.042) -0.019 (0.040) 0.207 10848 1047 0.207 10848 1047 0.206 10848 1047 0.206 10848 1047 0.206 10848 1047 0.027 (0.066) -0.056 (0.068) -0.028 (0.055) -0.013 (0.031) -0.018 (0.033) R-squared 0.150 0.151 0.150 0.151 0.150 0.150 0.150 Observations 10848 10848 10848 10848 10848 10848 10848 Clusters 1047 1047 1047 1047 1047 1047 1047 Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regression include; district fixed effects; geographic controls at the tehsil level, including distance to major river, dummy for tehsils boardering a major river, std. dev. of the tehsil's elevation, and mean tehsil elevation; and demographic controls including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Table 12: Impact of Flooding on Satisfaction with Government Relief References Acemoglu, Daron and James Robinson. 2001. “A Theory of Political Transitions.” American Economic Review 91(4):938–963. Acemoglu, Daron and James Robinson. 2012. Why Nations Fail. Crown Publishing. Achen, Christopher H. and Larry M. Bartels. 2004. Blind Retrospection: Electoral Responses to Drought, Flu, and Shark Attacks. Working paper Department of Politics, Princeton University. Agency for Technical Cooperation and Development. 2010. Rapid Needs Assessment: Upper Dir District — KPK Province. Report ACTED. Ahlerup, Pelle. 2011. Democratization in the Aftermath of Natural Disasters. Working paper University of Gothenburg. Altonji, Joseph G, Todd E Elder and Christopher R Taber. 2005. “Selection on Observed and Unobserved Variables: Assessing the Effectiveness of Catholic Schools.” Journal of Political Economy 113(1):151–184. Andrabi, Tahir and Jishnu Das. 2010. In Aid We Trust: Hearts and Minds and the Pakistan Earthquake of 2005. Working paper World Bank. Associated Press of Pakistan (APP). 2010. “Taliban urge government to reject US aid.” Pakistan Express Tribune. Bechtel, Michael M. and Jens Hainmueller. 2011. “How Lasting Is Voter Gratitude? An Analysis of the Short- and Long-Term Electoral Returns to Beneficial Policy.” American Journal of Political Science 55(4):851–867. Bellows, John and Edward Miguel. 2008. War and Local Collective Action in Sierra Leone. Working paper Department of Economics, University of California, Berkeley. Bellows, John and Edward Miguel. 2009. “War and Local Collective Action in Sierra Leone.” Journal of Public Economics 93(11–12):1144–1157. Berghold, Drago and Päivi Lujala. 2012. “Climate-related disasters, economic growth, and armed civil conflict.” Journal of Peace Research 49(1):147–162. Berrebi, Claude and Jordan Ostwald. 2011. “Earthquakes, hurricanes, and terrorism: do natural disasters incite terror?” Public Choice 149:383–403. Besley, Timothy and Robin Burgess. 2002. “The Political Economy of Government Responsiveness: Theory and Evidence from India.” Quarterly Journal of Economics 117(4):1415–1451. Besley, Timothy and Torsten Persson. 2011. “The Logic of Political Violence.” Quarterly Journal of Economics 126(3):1411–1445. Blair, Graeme, C. Christine Fair, Neil Malhotra and Jacob N. Shapiro. 2012. “Poverty and Support for Militant Politics: Evidence from Pakistan.” American Journal of Political Science . Blair, Graeme, Jason Lyall and Kosuke Imai. 2013. “xplaining Support for Combatants during Wartime: A Survey Experiment in Afghanistan.”. 59 Blattman, Christopher. 2009. “From Violence to Voting: War and Political Participation in Uganda.” American Political Science Review 103(2):231–247. Brancati, Dawn. 2007. “Political aftershocks: The impact of earthquakes on intrastate conflict.” Journal of Conflict Resolution 51(5):715–743. Brückner, Markus and Antonio Ciccone. 2011. “Rain and the Democratic Window of Opportunity.” Econometrica 79(3):923–947. Brückner, Markus and Antonio Ciccone. 2012. “Oil Price Shocks, Income, and Democracy.” Review of Economics and Statistics 94(2):389–399. Bullock, Will, Kosuke Imai and Jacob N. Shapiro. 2011. “Statistical Analysis of Endorsement Experiments: Measuring Support for Militant Groups in Pakistan.” Political Analysis 19:363– 384. Burke, Marshall B., Edward Miguel, Shanker Satyanath, John A. Dykema and David B. Lobell. 2009. “Warming increases the risk of civil war in Africa.” Proceedings of the National Academy of Sciences 106(49):20670–20674. Burke, Marshall, Solomon M. Hsiang and Edward Miguel. 2013. Quantifying the Climatic Influence on Human Conflict, Violence and Political Instability. Working paper University of California and Princeton University. Center for Research on the Epidemiology of Disasters (CRED). 2013. “the International Disaster Database (EM-DAT).” Electronic resource. Available at http://www.emdat.be/. Chen, Jowei. 2013. “Voter Partisanship and the Effect of Distributive Spending on Political Participation.” American Journal of Political Science 51(1):200–217. Cole, Shawn, Andrew Healy and Eric Werker. 2011. “Do voters demand responsive governments? Evidence from Indian disaster relief.” Journal of Development Economics 97:167–181. Dartmouth Flood Observatory (DFO). 2013. “Global Active Archive of Large Flood Events.” Electronic resource. Available at http://www.dartmouth.edu/~floods/Archives/index.html. Dhillon, Amrita and Susana Peralta. 2002. “Economic theories of voter turnout.” The Economic Journal 112(480):F332–F352. Fair, C. Christine, Neil Malhotra and Jacob N. Shapiro. 2012. “Faith or Doctrine: Religion and Support for Political Violence in Pakistan.” Public Opinion Quarterly . Feddersen, Timothy J. 2004. “Rational choice theory and the paradox of not voting.” The Journal of Economic Perspectives 18(1):99–112. Funk, Jeanne B., Robert Elliott, Michelle L. Urman, Geysa T. Flores and Rose M. Mock. 1999. “The Attitudes Towards Violence Scale: A Measure for Adolescents.” Journal of Interpersonal Violence 14(11):1123–1136. Gallego, Jorge A. 2012. Natural Disasters and Clientelism: The Case of Floods and Landslides in Colombia. Working paper Wilf Family Department of Political Science. 60 Gasper, John T. and Andrew Reeves. 2011. “Make It Rain? Retrospection and the Attentive Electorate in the Context of Natural Disasters.” American Journal of Political Science 55(2):340– 355. Gerber, Alan S. and Donald P. Green. 2012. Field Experiments: Design, Analysis, and Interpretation. New York: WW Norton. Ghimire, Ramesh and Susana Ferreira. 2013. Economic Shocks and Civil Conflict: The Case of Large Floods. Working paper University of Georgia. Ghosh, Biswajit. 2009. “NGOs, Civil Society and Social Reconstruction in Contemporary India.” Journal of Developing Societies 25(2):229–252. Gilligan, Michael J., Benjamin J. Pasquale and Cyrus D. Samii. 2011. Civil War and Social Capital: Behavior-Game Evidence from Nepal. Working paper Wilf Family Department of Politics, New York University. Green, Donald P., Alan S. Gerber and David W. Nickerson. 2003. “Getting Out the Vote in Local Elections: Results from Six Door-to-Door Canvassing Experiments.” Journal of Politics 65(4):1083–1096. Gronewold, Nathanial. 2010. “What Caused the Massive Flooding in Pakistan.”. Halvorson, S. J. and Jennifer Parker Hamilton. 2010. “In the aftermath of the Qa’yamat: the Kashmir earthquake disaster in northern Pakistan.” Disasters 34(1):184–204. Haque, Shamsul. 2004. “Governance based on partnership with NGOs: implications for development and empowerment in rural Bangladesh.” International Review of Administrative Sciences 70(2):271–290. Healy, Andrew and Neil Malhotra. 2009. “Myopic Voters and Natural Disaster Policy.” American Political Science Review 103(387-406). Healy, Andrew and Neil Malhotra. 2010. “Random Events, Economic Losses, and Retrospective Voting: Implications for Democratic Competence.” Quarterly Journal of Political Science 5(2):193–208. Jaeger, David, Esteban Klor, Sami Miaari and M. Daniele Paserman. 2012. “The Struggle for Palestinian Hearts and Minds: Violence and Public Opinion in the Second Intifada.” Journal of Public Economics 96(3-4):354–368. Khan, Riaz and Roshan Mughal. 2010. “Floods ravage NW Pakistan, kill 430 people.” Associated Press (AP). King, Gary, Christopher J. L. Murray, Joshua A. Salomon and Ajay Tandon. 2004. “Enhancing the Validity and Cross-Cultural Comparability of Measurement in Survey Research.” American Political Science Review 98(1):191–207. Kirsch, Thomas D., Christina Wadhwani, Lauren Sauer, Shannon Doocy and Christine Catlett. 2012. “Impact of the 2010 Pakistan Floods on Rural and Urban Populations at Six Months.”. Kolenikov, Stanislav and Gustavo Angeles. 2009. “Socioeconomic Status Measurement with Discrete Proxy Variables: Is Principal Component Analysis a Reliable Answer?” Review of Income and Wealth 55(1):128–165. 61 Kurosaki, Takashi, Humayun Khan, Mir Kala Shah and Muhammad Tahir. 2011. Natural Disasters, Relief Aid, and Household Vulnerability in Pakistan: Evidence from a Pilot Survey in Khyber Pakhtunkhwa. Primced discussion paper series, no. 12 Hitotsubashi University. Laufer, Avital and Zahava Solomon. 2006. “Posttraumatic Symtoms and Posttraumatic Growth Among Israeli Youth Exposed to Terror Incidents.” Journal of Social and Clinical Psychology 25(4):429–447. Lay, J Celeste. 2009. “Race, Retrospective Voting, and Disasters The Re-Election of C. Ray Nagin after Hurricane Katrina.” Urban Affairs Review 44(5):645–662. Looney, Robert. 2012. “Economic Impact of the Floods in Pakistan.” Contemporary South Asia 20(2):225–241. Miguel, Edward, Shanker Satyanath and Ernest Sergenti. 2004. “Economic Shocks and Civil Conflict: An Instrumental Variables Approach.” Journal of Political Economy 112(4):725–753. Mueller, Valerie, Clark Gray and Katrina Kosec. 2013. Long-Term Migration and Weather Anomalies in Pakistan. Working paper International Food Policy Research Institute. Narang, Vipin. 2013. “Posturing for Peace? Pakistan’s Nuclear Postures and South Asian Stability.” International Security 34:38–78. National Disaster Management Agency. 2011. Pakistan Floods 2010: Learning from Experience. Report NDMA. Nel, Philip and Marjolein Righarts. 2008. “Natural Disasters and the Risk of Civil Conflict.” International Studies Quarterly 52(1):159–185. Nolen-Hoeksema, Susan and Christopher G. Davis. 2002. Positive Responses to Loss: Perceiving Benefits and Growth. In Handbook of Positive Psychology, ed. C. R. Snyder and S. J. Lopez. New York: Oxford University Press pp. 598–607. Oak Ridge National Laboratory. 2008. “LandScan Global Population Database.” Electronic resource. Available at http://www.ornl.gov/landscan/. Office for the Coordination of Humanitarian Affairs (OCHA). 2010. Pakistan: Floods Relief and Early Recovery Response Plan. Flash appeal United Nations. URL: http://www.unocha.org/cap/appeals/revision-pakistan-floods-relief-and-early-recoveryresponse-plan-november-2010 Pande, Rohini. 2011. “Can Informed Voters Enforce Better Governance? Experiments in LowIncome Democracies.” Annual Review of Economics 3:215–237. Rahman, Sabeel. 2006. “Development, democracy and the NGO sector theory and evidence from Bangladesh.” Journal of Developing Societies 22(4):451–473. Ramsay, Kristopher W. 2011. “Revisiting the Resource Curse: Natural Disasters, the Price of Oil, and Democracy.” International Organization 65(3):507–529. Reeves, Andrew. 2011. “Political disaster: Unilateral powers, electoral incentives, and presidential disaster declarations.” The Journal of Politics 73(04):1142–1151. 62 Remmer, Karen L. 2013. “Exogenous Shocks and Democratic Accountability: Evidence from the Caribbean.” Comparative Political Studies . Righarts, Marjolein. 2010. “Pakistan’s floods: a window of opportunity for insurgents?”. Riker, William H. and Peter C. Ordeshook. 1968. “A Theory of the Calculus of Voting.” American Political Science Review 62(1):25–42. Shah, Aqil. 2013. “Constraining consolidation: military politics and democracy in Pakistan (20072013).” Democratization forthcoming. Shahbaz, Babar, Qasim Ali Shah, Abid Q. Suleri, Steve Commins and Akbar Ali Malik. 2012. Livelihoods, basic services and social protection in north-western Pakistan. Report Overseas Development Institute and Sustainable Development Policy Institute. URL: http://www.odi.org.uk/publications/6756-livelihoods-basic-services-social-protectionnorth-western-pakistan Shefter, Martin. 1977. “Party and Patronage: Germany, England, and Italy.” Politics & Society 7(4):403–451. Slettebak, Rune T. 2012. “Don’t blame the weather! Climate-related natural disasters and civil conflict.” Journal of Peace Research 49(1):163–176. Tedeschi, Richard G. and Lawrence G. Calhoun. 2004. “Posttraumatic Growth: Conceptual Foundations and Empirical Evidence.” Psychological Inquiry 15(1):1–18. United Nations Institute for Training and Research. 2003. “UNITAR’s Operational Satellite Applications Programme (UNOSAT).” Electronic resource. Available at http://www.unitar.org/ unosat/. United Nations Office for the Coordination of Humanitarian Affairs. 2010. Pakistan – Flood – July 2010 Table B: Total Humanitarian Assistance per Donor. Technical report Financial Tracking Service (FTS): Tracking Global Humanitarian Aid Flows http://fts.unocha.org. UNOCHA. 2013. Pakistan – Flood – July 2010 Table B: Total Humanitarian Assistance per Donor. Technical report Financial Tracking Service (FTS): Tracking Global Humanitarian Aid Flows http://fts.unocha.org. Varner, Bill. 2010. “Pakistan Flood Aid Helps Fight Terrorism as Peace ‘Fragile,’ Qureshi Says.” Bloomberg News . Velez, Yamil and David Martin. 2013. “Sandy the Rainmaker: The Electoral Impact of a Super Storm.” PS: Political Science & Politics 46(02):313–323. Voors, Maarten J., Eleonora E. M. Nillesen, Philip Verwimp, Erwin H. Bulte, Robert Lensink and Daan P. Van Soest. 2012. “Violent Conflict and Behavior: A Field Experiment in Burundi.” American Economic Review 102(2):941–964. Waraich, Omar. 2010. “Pakistan’s rich ’diverted floods to save their land.” The Independent. Ziring, Lawrence. 2009. Weak State, Failed State, Garrison State: The Pakistan Saga. In South Asias Weak States: Understanding the Regional Insecurity Predicament, ed. T.V. Paul. Stanford CA: Stanford University Press p. 181182. 63 Appendix (1) Independent % Area Variable: Flooded Panel A: Non-Militant Groups Tabliqhi Jamaat Flood Treatment (2) % Population Exposed (3) Pop. Exposed > Median (4) Pop. Exposed > 90th Percentile (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad -0.026 (0.105) 0.207* (0.121) 0.051 (0.049) 0.092 (0.065) 0.066* (0.040) 0.045** (0.020) 0.022 (0.022) -0.255 (0.230) -0.337* (0.195) -0.097 (0.088) -0.168 (0.115) 0.034 (0.074) 0.006 (0.043) 0.003 (0.041) -0.166 (0.145) -0.211 (0.150) -0.056 (0.068) -0.080 (0.089) 0.007 (0.051) -0.008 (0.029) 0.004 (0.029) -0.230* (0.122) -0.146 (0.128) -0.108** (0.054) -0.098 (0.071) -0.020 (0.062) -0.001 (0.035) -0.035 (0.036) -0.249 (0.156) 0.006 (0.058) -0.098 (0.070) -0.054 (0.058) -0.050* (0.030) -0.027 (0.037) Islamic Relief Flood Treatment 64 Aga Khan Flood Treatment Panel B: Militant Groups Jamaat-ud-Dawa (JuD) Flood Treatment Sipah-e-Sahaba Pakistan (SSP) Flood Treatment -0.331** (0.128) Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regressions include district fixed effects. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Appendix Table 1: Survey Recall on the Provision of Assistance to Internally Displaced People by Militant and Non-Militant Groups (1) (2) Independent Self-Reported Self-Reported Variables: Flood Exposure Affected Panel A: Asset Index (mean = 0.49, sd = 0.16) Flood Treatment -0.063*** (0.013) (3) Self-Reported Very | Extremely Bad -0.028*** (0.008) -0.035*** (0.007) R-squared 0.439 0.438 Observations 12178 12178 Clusters 1097 1097 Panel B:Monthly Household Income (log) (mean = 9.68, sd = 0.54) 0.439 12178 1097 Flood Treatment -0.034 (0.024) -0.075* (0.042) -0.036 (0.023) R-squared 0.291 0.291 0.291 Observations 11563 11563 11563 Clusters 1082 1082 1082 Panel C: Monthly Household Expenditures (log) (mean = 9.50, sd = 0.62) Flood Treatment -0.061 (0.043) -0.016 (0.024) -0.048* (0.025) R-squared 0.249 0.249 0.250 Observations 11708 11708 11708 Clusters 1084 1084 1084 Notes: Exposure measures calculated at the individual level. All regression include; tehsil fixed effects and demographic controls, including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Appendix Table 2: Impact of Flood Exposure on Household Assets, Income, and Expenditure 65 (1) (2) (3) (4) Independent % Area % Population Pop. Exposed > Pop. Exposed > Variable: Flooded Exposed Median 90th Percentile Panel A: Effectiveness of Junaid's/Mahir's Actions (mean = 0.65, sd in non-violent = 0.30, sd in violent = 0.38) No Controls β3: Violent * Flood 0.242** 0.306** 0.070* 0.127* (0.105) (0.123) (0.037) (0.076) Including Only District Fixed Effects β3: Violent * Flood 0.163* (0.091) 0.246** (0.105) 0.070** (0.034) 0.103* (0.062) 66 Including District Fixed Effects and Demographic Controls β3: Violent * Flood 0.194** 0.277*** 0.086*** 0.116** (0.086) (0.096) (0.033) (0.058) Panel B: Approval of Junaid's/Mahir's Actions (mean = 0.62, sd in non-violent = 0.31, sd in violent = 0.39) No Controls β3: Violent * Flood 0.251** 0.340*** 0.081** 0.180** (0.105) (0.122) (0.039) (0.074) Including Only District Fixed Effects β3: Violent * Flood 0.156* (0.094) 0.270** (0.109) 0.063* (0.035) 0.149** (0.062) (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad 0.167*** (0.055) 0.109*** (0.032) 0.071** (0.035) 0.104** (0.051) 0.074** (0.030) 0.037 (0.032) 0.127*** (0.049) 0.082*** (0.029) 0.057* (0.030) 0.190*** (0.059) 0.127*** (0.035) 0.087** (0.037) 0.132** (0.054) 0.100*** (0.032) 0.054 (0.033) Including District Fixed Effects and Demographic Controls β3: Violent * Flood 0.208** 0.320*** 0.086** 0.170*** 0.162*** 0.111*** 0.079** (0.087) (0.097) (0.034) (0.055) (0.052) (0.031) (0.032) Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Appendix Table 3: Impact of Flooding on Approval and Perceived Efficacy of Violent Protest with Different Sets of Control Variables 67 (1) (2) (3) (4) (5) (6) (7) Independent % Area % Population Pop. Exposed > Pop. Exposed > Self-Reported Self-Reported Self-Reported Variable: Flooded Exposed Median 90th Percentile Flood Exposure Affected Very | Extremely Bad Panel A: Effectiveness of Junaid's/Mahir's Actions If the Respondents assessed Government Relief Effort as Good β3: Violent * Flood 0.171 0.262 0.122*** -0.080 0.220*** 0.127*** 0.104*** (0.120) (0.167) (0.037) (0.091) (0.058) (0.036) (0.035) R-squared 0.278 0.277 0.283 0.277 0.284 0.283 0.282 Observations 5668 5668 5668 5668 5668 5668 5668 Clusters 892 892 892 892 892 892 892 If the Respondents assessed Government Relief Effort as Bad β3: Violent * Flood 0.186** 0.237*** 0.050 0.144*** 0.057 0.046 0.017 (0.090) (0.087) (0.043) (0.052) (0.060) (0.037) (0.038) R-squared 0.297 0.295 0.291 0.292 0.293 0.292 0.292 Observations 5719 5719 5719 5719 5719 5719 5719 Clusters 877 877 877 877 877 877 877 Panel B: Approval of Junaid's/Mahir's Actions If the Respondents assessed Government Relief Effort as Good β3: Violent * Flood 0.180 0.352** 0.129*** 0.020 0.269*** 0.160*** 0.131*** (0.126) (0.167) (0.042) (0.089) (0.064) (0.039) (0.038) R-squared 0.303 0.304 0.307 0.304 0.309 0.310 0.308 Observations 5668 5668 5668 5668 5668 5668 5668 Clusters 892 892 892 892 892 892 892 If the Respondents assessed Government Relief Effort as Bad β3: Violent * Flood 0.209** 0.264*** 0.054 0.169*** 0.070 0.065* 0.027 (0.084) (0.084) (0.042) (0.048) (0.061) (0.038) (0.039) R-squared 0.313 0.312 0.310 0.311 0.310 0.310 0.311 Observations 5719 5719 5719 5719 5719 5719 5719 Clusters 877 877 877 877 877 877 877 Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regression include; district fixed effects; geographic controls at the tehsil level, including distance to major river, dummy for tehsils boardering a major river, std. dev. of the tehsil's elevation, and mean tehsil elevation; and demographic controls, including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Appendix Table 4: Impact of Flooding on Approval and Perceived Efficacy of Violent Protest Based on the Respondents’ Assessment of the Government’s Relief Effort. (1) (2) Independent % Area % Population Variables: Flooded Exposed Panel A: Effectiveness of Junaid's/Mahir's Actions (mean = 0.65) (3) Pop. Exposed > Median (4) Pop. Exposed > 90th Percentile (5) Self-Reported Flood Exposure (6) Self-Reported Affected (7) Self-Reported Very | Extremely Bad 0.076 (0.111) 0.300* (0.169) 0.056 (0.039) 0.090 (0.070) 0.002 (0.043) 0.004 (0.076) 0.055* (0.032) 0.118** (0.058) 0.008 (0.021) 0.068* (0.035) 0.048** (0.019) 0.048 (0.032) R-squared 0.290 0.289 Observations 11963 11963 Clusters 1094 1094 Panel B: Approval of Junaid's/Mahir's Actions (mean = 0.62) 0.289 11963 1094 0.287 11963 1094 0.291 11963 1094 0.289 11963 1094 0.290 11963 1094 β2: Flood Treatment 0.077* (0.042) 0.021 (0.068) -0.080* (0.046) 0.071 (0.076) -0.005 (0.037) 0.123** (0.062) -0.034 (0.022) 0.084** (0.037) 0.020 (0.022) 0.056 (0.035) β2: Flood Treatment β3: Violent * Flood 68 β3: Violent * Flood 0.230** (0.106) 0.149 (0.156) 0.122 (0.118) 0.096 (0.159) -0.036 (0.121) 0.307* (0.174) R-squared 0.304 0.304 0.304 0.303 0.304 0.304 0.304 Observations 11963 11963 11963 11963 11963 11963 11963 Clusters 1094 1094 1094 1094 1094 1094 1094 Notes: Exposure measures calculated at the tehsil level in columns (1) - (4) and the individual level in columns (5) - (7). All regressions include: (vignette * district) fixed effects; geographic controls at the tehsil level, including distance to major river, dummy for tehsils boardering a major river, std. dev. of the tehsil's elevation, and mean tehsil elevation; and demographic controls, including gender, a head of household dummy, age, a literacy dummy, a basic numeracy dummy, education, and a Sunni dummy. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the primary sampling unit. Appendix Table 5: Impact of Flooding on Perceived Efficacy and Approval of Violent Protest with Vignette-District Fixed Effects (1) (2) (3) (4) (5) (6) Independent % Area Area Exposed > Area Exposed > % Population Pop. Exposed > Pop. Exposed > Variables: Flooded Median 90th Percentile Exposed Median 90th Percentile Panel A: Turnout Change (2013 - 2008) with Division Fixed Effects (mean = 0.11, sd = 0.08) Flood Treatment 0.112 (0.076) 0.038* (0.019) 0.016 (0.024) R-squared 0.315 0.323 0.302 Observations 129 129 129 Clusters 61 61 61 Panel B: First Differences ((2013-2008)-(2008-2002)) (mean = 0.08, sd = 0.13) Flood Treatment 0.207** (0.091) 0.071** (0.031) 0.057 (0.038) 0.166** (0.083) 0.008 (0.019) 0.055* (0.029) 0.327 129 61 0.301 129 61 0.320 129 61 0.266** (0.114) 0.037 (0.030) 0.073* (0.039) 0.027 129 61 0.028 129 61 0.047 (0.037) 0.071 (0.045) R-squared 0.054 0.064 0.025 0.057 Observations 129 129 129 129 Clusters 61 61 61 61 Panel C: First Differences ((2013-2008)-(2008-2002)) with Division Fixed Effects Flood Treatment 0.292** (0.146) 0.070* (0.035) 0.049 (0.042) 0.356** (0.163) R-squared 0.228 0.222 0.203 0.236 0.206 0.207 Observations 129 129 129 129 129 129 Clusters 61 61 61 61 61 61 Notes: Exposure measures calculated at the constituency level. All regressions include geographic controls at the constituency level, including distance to major river, dummy for constituencies boardering a major river, std. dev. of the constituency's elevation, and mean constituency elevation, as well as the proportion of constituency population exposed to the 2012 floods. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the district level. Appendix Table 6: Impact of Flooding on Turnout in the 2013 Pakistani National Assembly Elections in Constituencies Neighboring Major Rivers 69 (1) (2) (3) (4) (5) (6) Independent % Area Area Exposed > Area Exposed > % Population Pop. Exposed > Pop. Exposed > Variables: Flooded Median 90th Percentile Exposed Median 90th Percentile Panel A: Turnout Change (2013 - 2008) with Division Fixed Effects (mean = 0.10, sd = 0.08) Flood Treatment 0.109*** (0.039) 0.044*** (0.012) 0.022 (0.018) R-squared 0.319 0.328 0.294 Observations 209 209 209 Clusters 63 63 63 Panel B: First Differences ((2013-2008)-(2008-2002)) (mean = 0.07, sd = 0.13) Flood Treatment 0.185** (0.073) 0.077*** (0.026) 0.067 (0.041) 0.072 (0.056) 0.038** (0.015) 0.004 (0.022) 0.303 209 63 0.316 209 63 0.291 209 63 0.116 (0.115) 0.067** (0.027) 0.006 (0.045) 0.062 209 63 0.012 209 63 0.074*** (0.027) -0.006 (0.045) R-squared 0.075 0.087 0.029 0.029 Observations 209 209 209 209 Clusters 63 63 63 63 Panel C: First Differences ((2013-2008)-(2008-2002)) with Division Fixed Effects Flood Treatment 0.198*** (0.071) 0.078*** (0.024) 0.042 (0.032) 0.089 (0.111) R-squared 0.198 0.208 0.168 0.170 0.199 0.163 Observations 209 209 209 209 209 209 Clusters 63 63 63 63 63 63 Notes: Exposure measures calculated at the constituency level. All regressions include geographic controls at the constituency level, including distance to major river, dummy for constituencies boardering a major river, std. dev. of the constituency's elevation, and mean constituency elevation, as well as the proportion of constituency population exposed to the 2012 floods. Estimates significant at the 0.05 (0.10, 0.01) level are marked with ** (*, ***). Standard errors are clustered at the district level. Appendix Table 7: Impact of Flooding on Turnout in the 2013 Pakistani Provincial Assembly Elections in Constituencies Neighboring Major Rivers 70