I. Title page Title: Secondary pollutant formation in the Lake Tahoe Basin Subtheme this proposal is responding to Principal Investigator and Receiving Institution 3a: Secondary pollutant formation and the impact of TMDL-related primary and secondary atmospheric pollutants Barbara Zielinska Desert Research Institute 2215 Raggio Parkway, Reno, NV 89512 Phone: 775-674-7066 Fax: 775-674-7060 Email: Barbara.Zielinska@dri.edu Alan Gertler Desert Research Institute 2215 Raggio Parkway, Reno, NV 89512 Phone: 775-674-7061 Fax: 775-674-7060 Email: Alan.Gertler@dri.edu Andrzej Bytnerowicz US Forest Service, Pacific Southwest Research Station, Riverside, CA 92507 Phone: 951-680-1562 Fax: 951-680-1501 Email: abytnerowicz@fs.fed.us Wendy Goliff CE-CERT, University of California, Riverside 1084 Columbia Ave, Riverside, CA 92507 Phone: 951-781-5665 Fax: 951-781-5790 Email: wendyg@cert.ucr.edu Chad Praul Environmental Incentives 3351 Lake Tahoe Blvd, Ste 2, South Lake Tahoe, CA 96150 Phone: (530) 541-2980 Email: cpraul@enviroincentives.com Joel Burley Saint Mary’s College, Moraga, California Phone: 925-631-4839 Fax: 925-376-4027 Email: jburley@stmarys-ca.edu Shane Romsos TRPA 128 Market Street/Stateline, NV Phone: (775) 588-4547 Email: sromsos@trpa.org Charles Whitaker Desert Research Institute Phone: 440 279-4167, Fax: 775 674-7016 Email: charlesw@dri.edu $ 432,984 $ 108,248 Co-Principal Investigator Co-Principal Investigator Co-Principal Investigator Co-Principal Investigator Other Collaborators Agency Collaborator Grants Contact Person Funding requested: Total cost share (value of financial and in-kind contributions): II. Proposal Narrative a. Project abstract. The proposed study will characterize the precursors and pathways of secondary pollutant formation, including ozone (O3), secondary organic aerosol (SOA) and ammonium nitrate (NH4NO3) in the Lake Tahoe Basin. We will select a network of four strategic sampling sites inside the Basin to collect samples for detailed speciation of volatile organic compounds (VOC) and carbonyl compounds and measure concentrations of NH3, HONO, HNO3, SO2 and fine particulate NH4NO3 and (NH4)2SO4 with a resolution of several hours. We will also collect PM2.5 filter samples and continuously measure PM, O3 and NO/NO2 concentrations. These data will be used for development of an air quality model to predict ozone and other secondary pollutants formation in the Basin. The expected results from this proposed study will provide tools for evaluation of the present and future potential of O3, SOA and NH4NO3 formation as well as for interfacing with basin managers to support the development of sciencebased management strategies aimed at improving air quality and ecological sustainability of the Lake Tahoe Basin. In particular, the results of this study will be used to inform stakeholders which emissions should be more strictly regulated in order to attain air quality standards and reduce Total Maximum Daily Load (TMDL) pollutants delivered via the atmospheric deposition source category. b. Justification statement. Secondary pollutants are formed by chemical reactions in the atmosphere from precursors that are directly emitted from sources. Thus, the development of effective control strategies require detailed knowledge of the nature of the precursors, their sources and the processes that lead to their formation. Ozone is one of the most important secondary criteria pollutants, which concentrations currently exceed air quality standards in the Lake Tahoe Basin. PM2.5, another criteria pollutant, is composed mostly of secondary pollutants including ammonium nitrate, ammonium sulfate and secondary organic aerosol (SOA). The previous studies (Bytnerowicz et al., 2004; Dolislager et al., 2009a; Gertler et al., 2006) have shown that local generation of O3 and other pollutants in the Basin are likely to be more important than the long-range transport when it comes to exceedances of the state and national O3 standards and elevated levels of other pollutants within the Basin. However, until recently very little was known about the Basin’s spatial and temporal distribution of O3 and other secondary pollutant’s precursors such as nitrogen oxides (NOx), ammonia (NH3), and volatile organic compounds (VOC). Such information that is urgently needed for evaluating a potential for secondary pollutants photochemical generation in the Basin and developing recommendations for the air pollution control strategies, was completely lacking for VOCs, important precursors for O3 and SOA. We are presently conducting a study in the Lake Tahoe Basin (Bytnerowicz et al., 2010) that intends to supply more information regarding spatial distribution of O3 and its precursors. This study utilized a passive monitoring network of 34 sites inside and outside of the Basin. On a subset of 10 monitoring sites (mega sites), we also measured real-time O3 concentrations. The field part of this study was completed at the end of September 2010 and we are presently analyzing passive VOC, NOx, NH3 and nitric acid (HNO3) samplers and compiling continuous ozone data. The preliminary data shown for 10 mega sites during the July 14-29 period of the 2010 campaign indicate that among VOC, concentrations of biogenic species (isoprene, 2-methyl-3-buten-2-ol and a-pinene) are dominant (Figure 1). The highest concentration of all measured inorganic N gases (Figure 2) was determined at the nearlake Valhalla site located close to a very busy Highway 89. The lowest value of total inorganic N gases was at the remote Watson Creek site. Among the studied N species, NH3 and NO dominated at the lowelevation sites near the Lake (Blackwood Canyon, Genoa 7000, Sugar Pine Point, Thunderbird and Valhalla), and the proportion of NO2 and nitric acid (HNO3) was lower (an indication of direct effects of the fuel combustion emissions). The diurnal O3 concentrations (Figure 3) show strong diurnal pattern (i.e. max concentrations during the day hours, 0900 to 1700 hr with min at night and early morning ) for 5 of the 10 sites (Valhalla, Watson Creek, Sugar Pine, Blackwood Canyon, Genoa 7000 feet), nearly flat concentrations over the whole 24 hrs for 3 remote sites (Genoa 9000 feet, Upper Incline and Angora Lookout) and intermediate diurnal patters for the remaining 2 sites (Genoa 8000 feet and Thunderbird). This may indicate a strong influence of nighttime O3 titration by fresh NO auto emissions at the 5 sites 2 with large diurnal variations and enhanced regional O3 transport to the 3 high elevation “flat ozone” sites. However, most of the 34 sites at the present study were intentionally selected to be situated away from any urban centers to characterize regional O3 and its precursor distribution. In addition, the present study will not supply the information regarding temporal variability of O3 precursors, as only two-week integrated passive samples were collected. Also, only selected, limited subset of VOC was monitored, due to the inherent limitation of the passive VOC method. This proposed study intends to address these gaps in the current understanding of the chemical environment of the Lake Tahoe Basin. We will build on the results of our current studies (Bytnerowicz et al., 2010) to select the network of four strategic sampling sites inside the Lake Tahoe Basin to collect samples for detailed speciation of VOC and carbonyl compounds (important O3 and SOA precursors) and monitor O3, NOx, NH3, ammonium nitrate and sulfate (NH4NO3 and (NH4)2SO4), and HNO3 concentrations with enhanced temporal resolution. We will also collect PM2.5 filter samples and monitor total PM2.5 mass continuousl . These data will be used for the implementation of an air quality model to predict ozone and other secondary pollutants formation in the Basin. The expected results from this proposed study will greatly enhance the results obtained in our current study and provide tools for evaluation of the present and future potential of O3, SOA, NH4NO3 and (NH4)2SO4 formation as well as for developing science-based management strategies aimed at improving air quality and ecological sustainability of the Lake Tahoe Basin. In particular, the results of this study will inform basin managers which precursor emissions should be more stringently regulated in order to attain and maintain Environmental Threshold Carrying Capacities (i.e. TRPA Threshold Standards) and to develop appropriate and effective control strategies which can reduce TMDL-related pollutant loads. c. Concise background and problem statement. Ozone: O3 is a secondary criteria pollutant that is not directly emitted from sources, but formed by chemical reactions in the atmosphere. In order to control O3 levels in the Lake Tahoe Basin, it is necessary to understand the underlying chemistry of O3 formation. The factors to consider are nitrogen oxides (NOx = NO + NO2) and volatile organic compounds (VOCs). NO reacts with O3 to produce more NO2 in a process that is only limited by the availability of O3. During the daylight hours NO2 decomposes photochemically to reproduce NO. The ratio between NO and NO2 is governed by the photolytic rate J{NO2}. The photolysis of NO2 leads to the formation of O3. Since O3 is removed by the reaction with NO and is produced via the photochemical reaction, it seems that the net production of O3 would be NO2 limited. However, through a series of reactions involving NO, VOCs, and the hydroxyl radical (OH), additional NO2 is formed, which can subsequently photolyze to generate O3 via a chain reaction mechanism. This chain reaction is eventually terminated by a process that yields nitric acid (HNO3). Thus, the chemical processes involving NOx and VOCs leading to O3 formation in the Lake Tahoe Basin also result in the formation of HNO3, an important contributor to the overall deposition of N and NH4NO3 formation. Different types of hydrocarbons react at different rates and with a variety of oxidants based on their structure and composition. Each VOC species has its own unique reaction rate in the atmosphere. Some VOCs have an atmospheric lifetime of a few days (e.g., benzene), and contribute little to O3 formation on a local scale. Others, such as isoprene, have a lifetime of a few hours, and can lead to significant O3 formation on a local scale. The mechanism of degradation for each VOC is also important. VOCs such as benzaldehyde (formed from the degradation of toluene) consume radical species in the atmosphere, thereby reducing O3 formation. Conversely, VOCs such as formaldehyde and glyoxal form large numbers of radicals during their degradation in the atmosphere, increasing the rate of O3 formation. For these reasons, it is important for O3 modeling to have as much information regarding the composition of VOCs in the atmosphere as possible. Secondary Organic Aerosol (SOA). Organic carbon constitutes a large portion of PM2.5 in the basin (Engelbrecht et al., 2009) which is an important contributor to visibility degradation. Organic aerosols are complex mixtures of directly emitted or primary organic aerosol (POA) and secondary organic aerosols (SOA) derived from chemical reactions and gas-to-particle conversion of VOC emitted 3 by both anthropogenic and natural sources. Recent field studies indicate that SOA is significantly more abundant than state-of-the-art SOA models predict (de Gouw et al., 2005; Heald et al., 2005; Johnson et al., 2006). Hence, the atmospheric relevance and contributions of the different SOA formation pathways and associated chemical reactions mechanisms still remain to be clarified (Fuzzi et al., 2005). Oxidation of biogenic emissions is believed to the dominant source of SOA globally, mostly by ozonolysis of terpenes (Jenkin, 2005). However, Volkamer et al. (2006) showed that in the real urban atmosphere reactive anthropogenic VOCs produce significant amounts of SOA. The contribution of biogenic and anthropogenic hydrocarbons to SOA in the Lake Tahoe Basin is presently unknown. Although we measured selected VOC with passive samplers during our summer 2010 field study at the 34 sites in the Lake Tahoe Basin (Bytnerowicz et al., 2010), the measurements were averaged over 2-week periods and the list of compounds was limited. For modeling SOA and ozone concentrations the more complete VOC species list and much better time resolution is needed. Ammonium nitrate and sulfate. Ammonium nitrate (NH4NO3) and sulfate [(NH4)2SO4] are rather minor constituents of PM2.5 in the Lake Tahoe Basin (Engelbrecht et al., 2009). However, due to the importance of nitrogen deposition to the Lake and potential artifact connected with filter nitrate measurements, we propose to monitor precursors of NH4NO3 including ammonia, NOx and HNO3. Because passive samplers offer only a possibility of longer-term measurements (weeks), we propose to use a combination of NO/NOx UV absorption monitors (2B Technologies, Boulder CO) and honeycomb denuder & filter pack systems (Koutrakis et al., 1994). We will be able to measure concentrations of NO, NO2, NH3, HONO, HNO3, SO2 and fine particulate NH4, NO3 and SO4 with a resolution of several hours. Atmospheric Air Quality Model. In order to provide meteorological input to the photochemical model, we will simulate selected cases with monitoring data collected during the field campaign portion of this project using an appropriate meteorological model such as Mesoscale Model 5 (MM5) (Grell et al., 1994) or the Weather Research and Forecasting Model (WRF) (Michalakes et al., 2001). Both models listed output on a 3D grid includes air temperature, humidity, wind components, and turbulence kinetic energy, with multiple-nest capabilities, nonhydrostatic dynamics, 4-D data assimilation capability, a number of physics options, and portability to a wide range of computer platforms. Atmospheric flows in the Lake Tahoe Basin are fairly complex due to developed topography and interactions of the regional and local flows that significantly influence fate of air pollutants in the basin. A lack of dense meteorological measurements at the surface and aloft represents an additional challenge in understanding details of the atmospheric flows and stability in the basin. Consequently, only complex meteorological models such as MM5 or WRF can provide sufficient information as input to the photochemical model. Due to complexity of the terrain, we will simulate case studies with sufficient horizontal (1 km) and vertical resolution (15-20 points) in the planetary boundary layer. Prior to any analysis, model results will be evaluated using available meteorological data in the basin and vicinity. Model outputs will be stored in hourly intervals and processed as inputs to the CAMx photochemical model. The Comprehensive Air Quality Model with Extensions (CAMx) modeling system was developed by the ENVIRON International Corporation and is based on the Urban Airshed Model in order to address needs mandated by the Clean Air Act Amendments in 1990 (Byun and Schere, 2006). CAMx is an Eulerian grid photochemical model that treats multiple pollutants at multiple atmospheric levels using a “one-atmosphere” multiscale approach. It provides a fully modular framework linked with emissions estimation and prognostic meteorological models. Its multi-scale capability is supported with a generalized coordinate system consistent with many meteorological models and enables users to apply nesting to investigate local and regional air pollution phenomena. The multi-pollutant approach of CAMx makes it suitable for applications of trapospheric ozone formation, particulate matter, acid deposition, and toxics through use of gaseous and aqueous chemistry and modal aerosol dynamics. CAMx allows users to choose from different chemical mechanisms including CB-IV (Gery et al., 1989), CB05 (Yarwood et al., 2005), and SAPRC99 (Carter, 2000). Each of these mechanisms is supported with additional aerosol and toxic chemistry. For emissions input, we will use the emissions inventory database developed by Gertler et al. (2008) which is the most up-to-date emissions database of its kind. 4 d. Goals, objectives, and hypotheses to be tested Main Goals: 1. Identify the precursors and pathways leading to the formation of secondary pollutants, including ozone, NH4NO3, (NH4)2SO4 and SOA 2. To employ the air quality model CAMx to predict the formation of O3, SOA, (NH4)2SO4 and NH4NO3. Model output will be compared to observations made during the field campaign portion of this project to assess the model’s capabilities and potential biases. 3. Provide information for important policy decisions designed to reduce air and water impacts of atmospheric pollutants. Specific Objectives: 1. Based on the results of the 2010 summer study (Bytnerowicz et al., 2010) select up to four sites in the Lake Tahoe Basin for the 5-days (including weekdays and weekend) intensive air quality study 2. Conduct the air quality measurements in the Lake Tahoe Basin to quantify VOC, carbonyl compounds, NH3, HNO3, particulate NH4, NO3 & SO4, and PM2.5 with sub-daily resolution 3. Determine real-time concentrations of O3 and NO/NO2 in these sites with portable absorption monitors. 4. Employ the air quality model CAMx to predict O3 for the Lake Tahoe Basin. 5. Employ the air quality model CAMx to predict SOA, (NH4)2SO4 and NH4NO3 for the Lake Tahoe Basin. 6. Communicate the results of this study to the managers and the public Hypotheses to be tested: 1. The majority of precursors for O3 formation come from in-basin sources. 2. The majority of precursors for SOA formation come from in-basin sources. 3. Out-of-basin contribution to observed O3 and SOA levels is limited. 4. To control O3 formation, one needs to develop policies to limit NOx emissions. 5. Reduction on O3 levels will reduce the amount of SOA. e. Approach, methodology and location of research This study is planned for two years. The first year (2011/2012) will be devoted to field measurements and chemical analyses and the second year (2012/2013) to data processing, models development/validation and writing reports and scientific papers. Monitoring network: Based on the preliminary results of our current Lake Tahoe Basin study (see Figures 1, 2 and 3) we will establish four sampling sites in the Lake Tahoe Basin. Two of these sites will be situated at high elevation on the west and east sites of the Basin (for example Genoa 9000 feet, top of the Heavenly transect at about 10000 ft, top of the Homewood ski resort) and two will be at the Lake level, close to the major population activities (for example Valhalla and Sugar Pine State Park, South Lake Tahoe Airport, Thunderbird or Cave Rock sites). The final decision as to the appropriate selection of the sampling sites will be made after discussion with the project managers, taking into account the sampling logistics. We will conduct 5-days (including weekdays and weekend) intensive air quality study with canisters and DNPH cartridges for VOC collection and NH3, HONO, HNO3, SO2, particulate NH4, NO3 and SO4, NOx, O3 and PM2.5 monitoring. We will collect three samples per day: one at the morning during max ozone concentration changes (0600 to 0900), one at the max ozone concentrations (1000 to 1700) and one overnight (1800-0500). Ozone and NO/NO2 will be monitored continuously and we will also use DustTrak (TSI Incorporated) for continuous PM monitors in some sites in addition to filter PM sampling. We will select a period in July or August, based on the forecast of sunny and warm conditions that are conducive to O3 and SOA formation. VOC measurements: Hydrocarbons in the C2 to C12 range will be collected using 6 L passivated stainless steel SUMMA canisters and analyzed according to the EPA Method TO-15 using a Varian 3800 gas chromatograph interfaced to a Varian Saturn 2000 ion trap mass spectrometer (MS) and flame 5 ionization detector (FID). Approximately 80 anthropogenic and biogenic species will be measured (Zielinska et al., 2001, 2003; Fujita et al., 2003). Carbonyl compounds will be collected using Sep-Pak cartridges which have been impregnated with an acidified 2,4-dinitrophenylhydrazine (DNPH) reagent (Waters, Inc), according to the EPA Method TO-11A. The cartridges will be analyzed with a Waters 2690 high performance liquid chromatograph (HPLC) equipped with a photodiode array detector for separation and quantification of the hydrazones (Zielinska et al., 2001, 2003; Fujita et al., 2003). PM2.5 measurements. PM2.5 will be collected using medium volume 2-channel filter samplers (113 Lpm sampling rate) with 47-mm Teflon (for PM2.5 mass) and quartz filters for organic and elemental carbon (OC/EC) and ions measurements (Chow et al., 1993). In addition, battery operated DustTrak (TSI) will be used at some sites for continuous PM measurements. Ozone measurements: The real-time O3 concentrations will be obtained with portable UV absorption 2B Technologies monitors (Bognar and Birks, 1996). N inorganic gases measurements: A compact 12V NO monitor (2B Technologies) with NO2 converter (Model 401) will be used for two sites with limited power and the other two sites will be using standard chemiluminescence Monitor Labs instruments. Honeycomb denuder/filter pack systems will be used for collection of NH3, HONO, HNO3 SO2, and particulate NH4, NO3, and SO4. Acidic gases (HONO, HNO3 and SO2) are collected on a honeycomb denuder coated with carbonate, glycerin and methanol solution; NH3 on citric acid, glycerin and methanol solution, and fine (<2.5 µm) particulate NH4, NO3 and SO4 on a filter pack consisting of Teflon nylon and citric acid collated glass filters. Coarse particles (>2.5 µm diameter) are removed on an impaction plate. These systems are connected to steady flow pumps moving air through the assembly at 10 l/min (Koutrakis et al., 1993). Model Development: Use MM5 or WRF meteorological output as input into CAMx for the Lake Tahoe Basin. Also, obtain emissions inventories for necessary model input. Data obtained from the field campaign will be used for both initial conditions and test model output. f. Relationship of the research to previous and current relevant research, monitoring, and/or environmental improvement efforts The proposed research is a logical continuation of the previous efforts focusing on understanding air quality and its effects on the human health-based national and state air pollution standards, and also on potential ecological impacts of air pollution and atmospheric deposition in the Lake Tahoe Basin (Bytnerowicz et al., 2010, 2004; Dolislager et al. 2009a, b; Gertler et al, 2006; Koracin et al., 2004; Tarney et al, 2001a, b; 2005). This research will be conducted by a team consisting of researchers and air quality specialists of the Desert Research Institute, US Forest Service, University of California, Riverside, Environmental Incentives, LLC, and St. Mary’s College of California. Most of these team members are involved in the current Lake Tahoe study (Bytnerowicz at al., 2010). A key aspect of this work will be interfacing with basin managers to communicate the findings in order to aid with the development of strategies to reduce the levels of pollutants leading to reduced air quality (i.e., O3), visibility (i.e., SOA) and water quality (i.e., nitrogen deposition). g. Strategy for engaging with managers and obtaining permits This research team will engage a core group of stakeholders to provide early scope and product input, and review draft research products. During the course of the project stakeholders will receive interim updates that are targeted to their needs and will help them understand the research process. One particularly relevant product of the research will be a management-oriented summary of findings that will consider how available data and products should influence future decisions on how to meet Environmental Threshold Carrying Capacities (e.g. Visibility) and other resource management issues such as TMDL load reductions for the atmospheric deposition source category. After results are quality assured, they will be submitted to relevant journals for peer review and publication. 6 Engagement Strategy Timeframe Convene key manager/user stakeholder group Meeting 1: understand project objectives and provide management questions Meeting 2: discuss interim results and necessary adjustments Meeting 3: review draft results and products Provide interim updates to stakeholder group via email or phone call Develop management-oriented Summary of Findings Memo Present results at relevant local venue open to all managers and the public project initiation mid-project project conclusion quarterly project conclusion project conclusion h. Description of deliverables/products and plan for how data and products will be reviewed and made available to end users The proposed study will produce: 1. Final Report - including the following information:: • detailed information on approximately 80 VOC concentrations, including biogenic and anthropogenic ozone, NH4NO3 and SOA precursors in four sites in the Lake Tahoe Basin with a few hour resolution over a five days period (weekend and weekdays) • detailed information on carbonyl compound concentrations, which have not been measured in the Tahoe Basin before and are important precursors of ozone and SOA formation • detailed information on NOx, HNO3, NH3 and other secondary pollutant precursors 2. Air Quality Model that predicts ozone, SOA and other secondary pollutants formation in the Basin 3. Progress Reports - delivered quarterly and yearly including all information specified in the request for proposals 4. At least 2 research papers to be published in high quality peer-reviewed journal 5. Summary of Findings – a brief memo oriented toward resource managers who will be able to use the information to make better informed decisions about topics relating to secondary air quality pollutants. Potential topics that may be related include attainment of standards for criteria air pollutants, deposition of TMDL pollutant species to Lake Tahoe and acceptable levels of emission sources. The format of the memo will focus on bulleted information and functional data graphics presented in just a few pages of the most relevant results. Plan for how data and products will be reviewed and made available to end users: Data and knowledge developed with these funds will be reviewed and transferred to several types of end users through targeted methods. Technical users such as future researchers will have access to quality assured data in useable formats such as Microsoft Excel tables or CSV files. Resource managers will be able to provide input through in-person meetings and enhance their knowledge through reading a summary of findings and attending presentations by the team. All users including the public will have access to final products through postings on relevant websites such as TIIMS.ORG. Specifically: Review Strategy Timeframe Stakeholder group review through in-person presentations and written comment on draft products Develop management-oriented summary of findings for long-term reference Post final products to TIIMS.ORG and other relevant websites as recommended by the stakeholder group; postings will include quality assured datasets in a form that can be used for future analysis Present results at relevant local venue open to all managers, executives and public Submittal of at least 2 papers to peer-reviewed journal 7 final months project conclusion quarterly project conclusion project conclusion III. Schedule of major milestones/deliverables Milestone/Deliverables Start Date End Date Description Meeting with the program managers and other stakeholders Preparation for field study June 2011 June 2011 Initial meeting to discuss project objectives and technical approach 7/1/2011 7/15/2011 Field study 07-08/ 2011 07-08/ 2011 Sample analysis Aug 2011 Nov 2011 Assemble and validate all field data Model development Dec 2011 Feb 2012 Feb 2012 June 2012 Run and validate model Prepare progress reports June 2012 October 2011 Nov 2012 Jan 2013 Annual accomplishment report Prepare draft final report Aug 2012 Sept 2012 Jan 2013 March 2013 Prepare final report May 2013 June 2013 Prepare and submit peerreviewed papers June 2013 Dec 2013 Sites selection, sampling media preparation, logistic coordination Conduct 5 days field study in 4 sites, collect time integrated samples and continuous data Analyze collected canister, DNPH cartridges, filters, denuders and filter’s packs Validate all data and deliver them for model development and validation Develop models for ozone, SOA and NH4NO3 formation Run models for various scenarios Submit brief progress report to Tahoe Science Program coordinator by the 1st of July, October, January, and April. Prepare annual summary of accomplishments in September. Prepare and submit draft final report for agency review Prepare final report responding to agency’s comments Prepare and submit minimum 2 peer-reviewed papers 8 IV. Literature cited/References Bytnerowicz, A., Fenn, M., Gertler, A, Preisler, H. and Zielinska, B., 2010. Distribution of ozone, ozone precursors and gaseous components of atmospheric nitrogen deposition in the Lake Tahoe Basin, Proposal submitted to U.S. Department of Agriculture Forest Service, Pacific Southwest Research Station, funded by Tahoe SNPLMA Science Program, contract No P063 Bytnerowicz, A., Arbaugh, M, and Padgett, P., 2004. Evaluation of ozone and HNO3 vapor distribution and ozone effects on conifer forests in the Lake Tahoe Basin and eastern Sierra Nevada. Final Report to California Air Resources Board, Contract No. 01-334, USDA Forest Service, Pacific Southwest Research Station. Byun, D. and Schere, K.L., 2006. Review of the Governing Equations, Computational Algorithms, and Other Components of the Models-3 Community Multiscale Air Quality (CMAQ) Modeling System. Mechanics Review 59, 51-77. Carter, W.P.L., 2000. Implementation of the SAPRC-99 Chemical Mechanism into the Models-3 Framework. Final Report to U.S. EPA. Chow, J.C., Watson J.G., Pritchett L.C., Pierson W.R., Frazier C.A. and Purcell, R.G. , 1993: The DRI thermal/optical reflectance carbon analysis system: description, evaluation and applications in U.S. air quality studies. Atmos. Environ., 27A, 1185-1202. Dolislager, L. J., VanCuren, R., Pederson, J. R., Lashgari, A., McCauley, E. 2009a. An assessment of ozone concentrations within and near the Lake Tahoe Air Basin. Atmospheric Environment doi:10,1016/j.atmosenv.2009.07.017. Dolislager, L. J., VanCuren, R., Pederson, J. R., Lashgari, A., McCauley, E. 2009b. A summary of the Lake Tahoe Atmospheric Deposition Study (LTADS). Atmospheric Environment doi:10,1016/j.atmosenv.2009.09.020.. de Gouw, J. A.; Middlebrook, A. M.; Warneke, C.; Goldan, P. D.; Kuster, W. C.; Roberts, J. M.; Fehsenfeld, F. C.; Worsnop, D. R.; Canagaratna, M. R.; Pszenny, A. A. P.; Keene, W. C.; Marchewka, M.; Bertman, S. B.; Bates, T. S. 2005. Budget of organic carbon in a polluted atmosphere: Results from the New England air quality study in 2002, J. Geophys. Res. 110, D16305.Heald et al., 2005 Engelbrecht J., A Gertler and T. VanCuren ,2009. Lake Tahoe Source Attribution Study (LTSAS): Receptor Modeling Study to Determine the Sources of Observed Ambient Particulate Matter in the Lake Tahoe Basin, Final Report to USDA Forest Service Pacific Southwest Research Station, September 2009 EPA Method TO-11A: Determination of formaldehyde in ambient air using adsorbent cartridge followed by high performance liquid chromatography; U.S. Environmental Protection Agency: Cincinnati, 1999. EPA Method TO-15: Determination of volatile organic compounds in air collected in specially-prepared canisters and analyzed by gas chromatography/mass spectrometry; U.S. Environmental Protection Agency: Cincinnati, 1999. Fujita, E. M., D. E. Campbell, B. Zielinska, J. C. Sagebiel, J. L. Bowen, W. S. Goliff, W. R. Stockwell, and D. R. Lawson , 2003. Diurnal and Weekday Variations in the Source Contributions of Ozone Precursors in California’s South Coast Air Basin, J. Air Waste Manage. Assoc., 53, 844-863. Fuzzi S., M.O. Andreae, B.J. Hubert, M. Kulmala, T.C. Bond, M. Boy, S.J. Doherty, A. Gunther, M. Kanakidou, K. Kawamura, V-M Kerminen, U. Lohmann, L.M. Russel and U. Pooschi, 2005. Critical assessment of the current state of scientific knowledge, terminology, and research needs concerning the role of organic aerosols in the atmosphere, climate, and global changes. Atmos. Chemistry and Physics Discussions, 5,11729-11780 Gertler, A.W., A. Bytnerowicz, T.A. Cahill, M. Arbaugh, S. 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Figures Sampling Period July 14-29 4 bz124m n_dec 3 a_pinen ppbv n_non styr 2 mp_xyl etbz n_oct 1 tolue MBO cyhexa K benze n_hex W A TS O N CR EE AL LA E LH VA ER PP U U ND IN ER R TH CL IN BI RD E PI N 00 ' G A SU O A 90 00 ' G EN O A 80 00 ' 70 G EN W O O A G EN B LA A CK NG O R O D A 0 i_prene bud13 Figure 1. Passive VOC concentrations (selected biogenic and anthropogenic species) measured over 2week period at 10 sites; bud13=1,3-butadiene; i-prene=isoprene; n_hex=n-hexane; benze=benzene; cyhexa=cyclohexane; MBO=2-methyl-3-buten-2-ol; tolue=toluene; n_oct=n-octane; etbz=ethylbenzene; mp_xyl=m&p-xylene; styr=styrene; n_non=n-nonane; a_pinen=alpha-pinene; n_dec=n-decane; bz124m=1,2,4-trimethylbenzene 11 Inorganic gaseous N apportionment, July 14-29, 2010 8 HNO3 NO2 NO NH3 7 6 -3 N (mg m ) 5 4 3 2 1 Cr ee k on at s Va lh al la nc lin e er I W Up p de rb ird Th un Pi ne 0 Su ga r a 90 0 0 Ge no Ge no a 80 0 0 70 0 Ge no a d w oo Bl ac k An go ra 0 Figure 2. Inorganic gaseous nitrogen species measured over 2-weeks with passive methods Sampling Period July 14-29, 2010 60 50 Angora ppbv 40 Blackwood Genoa 7000 Genoa 8000 Genoa 9000 30 Sugar Pine Thunderbird Upper Incline 20 Valhalla Watson Creek 10 0 0 2 4 6 8 10 12 14 16 18 20 22 Hour Figure 3. Diurnal ozone concentrations averaged over 2-week period measured with continuous ozone monitors at the 10 sites 12