Arjumand-Habib - Divecha Centre for Climate Change

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Climate Change: Bangladesh Perspective

Arjumand Habib, Director

Bangladesh Meteorological Department

Dhaka, Bangladesh

1. Introduction

Geographically Bangladesh is in the highly disaster prone area of deltaic origin of Ganges-

Brahmaputra Basin having Himalayas in the north and Bay of Bengal in the south with a complex coastal configuration and shallow bathymetry. It is an agro-based tropical country, climate is southwest monsoon driven with a significant variation in rainfall and temperature over the year. Recorded tropical cyclone devastation in Bangladesh is the worst in the world. About

80% of the land is flood prone, 90% discharge of Ganges-Brahmaputra-Meghna basin is through Bangladesh during monsoon. Other than tropical cyclone, extreme events like thunderstorms, tornadoes and localized heavy rainfall causing causalities and loss which is almost close to that of one cyclone every year. With this climate change impact would adversely affect the existing vulnerability more. As a least developed country with highest population density (Total area of Bangladesh 143,999 square kilometers; according to the latest census report published in July 2011 population density is 964 per square kilometer; the rate of population growth is 1.34 per year and total number population increased during last 10 years is about 1.8 crore ), inadequate infrastructure for protection, lack of institutional capacity for taking proper adaptation and mitigation and because of its climate sensitive economy, particularly agriculture will face enormous human suffering in terms of food, water, shelter, health and overall livelihood. Expansion and strengthening of capacity in generation and utilization of emerging climate information and provision of effective end-to-end early warning are the urgent need to support Government, private sectors, NGO’s and public for disaster risk reduction and for adaptation and mitigation of climate change impact.

2. Climate and Climate Change

2.1 Climate of Bangladesh

Bangladesh is a subtropical monsoon climate characterized by wide seasonal variations in rainfall, moderately warm temperatures, and high humidity. Based on the analysis of pressure, rainfall and temperature, the climate of this country can be described under the following four seasons: a. Winter or Northeast Monsoon: This season comprises of December, January and

February; mean temperature is 1821°C and average rainfall is about 1.5% of the total annual rainfall. b. Summer or Pre-Monsoon: This season consists of March, April and May; average rain fall is 17% and mean temperature is 23-30 °C and average rainfall is 17% . c. Southwest Monsoon or Monsoon: This season consists of June, July, August and

September; average rain fall of this season is about 72.5% of the total annual rainfall. d.

Autumn or Post-Monsoon: This season consists of October and November; average rainfall receives in this season is about 9%.

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3. Trend of Change

3.1 Temperature: Temperature trends during last 60 years (1950-2010) based on observed data of BMD, minimum temperature and maximum temperature both have a tendency to increase, minimum more making average day temperature to follow rising trends as given in

Fig. 1 and Fig. 2.

31.5

31.0

y = 0.0092x + 30.234

R

2

= 0.2235

30.5

30.0

29.5

29.0

Fig: 1: Temporal variation of annual maximum temperature of Bangladesh during 1950-

2010

22.0

21.8

21.6

21.4

21.2

21.0

20.8

20.6

20.4

20.2

20.0

y = 0.0107x + 20.677

R

2

= 0.3359

Fig: 2: Temporal variation of annual minimum temperature of Bangladesh during 1950-

2010

3.2 Rainfall: Average rainfall during last 60 years (1950-2010) has a positive trend with a slight decrease in monsoon season.

2

3000

2800

2600

1600

1400

1200

1000

2400

2200

2000

1800 y = 1.048x + 2224.9

R

2

= 0.0043

Fig. 3: Temporal variation of annual rainfall of Bangladesh during 1950-2010

20 y = -0.0616x - 5.1577

R

2

= 0.0082

10

0

-10

-20

-30

-40

Fig. 4: Inter-annual variation of monsoon rainfall in Bangladesh during 1951-2010

Under a collaborative research between SAARC Meteorological Centre (SMRC) and Nagoya

University on the ‘Understanding the rainfall climatology and detection of extreme weather events in SAARC region’ has done in two phases. For rainfall climatology Tropical Rainfall

Measuring Mission (TRMM) data sets and for generation of extreme events RegCM (Regional

Climate Model) have been used for Bangladesh and the model simulated events are compared with BMD’s observed data sets. Increasing rate of wet days is high in the NE and SE regions of

Bangladesh. Regarding temperature both maximum and minimum have a rising trends, minimum more over maximum, maximum more or less stable. So both the analysis shows the signature of Global Warming.

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3.3 Extreme events

Tropical cyclone intensity analysis shows that since 1876 onward particularly in the last 20 years frequency and the intensity of cyclone more than 200 km/hour has an increasing trend.

Also other extreme events like heavy rainfall within short scale of time causing flash flood in pre-monsoon period are increasing and added extra pressure on monsoon flooding especially in urban area drainage congestion, prolonged water logging and landslides in the hilly region and also accelerate river erosion.

Fig. 5: Intense Cyclones (wind speed more than 200 Km/h) over Bay of Bengal during 1876 -

2010

Fig. 6: Intense Cyclones (wind speed more than 200 Km/h) over Bay of Bengal during 1950 -

2010

During 1876 – 1964 there was only one intense cyclone (wind speed more than 200 Km/h) over

North Bay of Bengal but in next 45 years (1965 – 2010) it was 9. From 1950 to 1990 intense cyclones were only two but during next 20 years (1991-2010) it was 7.

3.4 Rainfall intensity

Pre-monsoon season: Frequency of heavy rainfall are increasing in March (+0.0048/year) and

April (+0.0061/year) but significant increasing trend (0.0258/year) is observed in May.

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Therefore, heavy rainfall during pre-monsoon season has considerable increasing trend

(+0.0258/year) which means extreme weather is increasing.

Monsoon Season: Frequency of heavy rainfall are increasing in June (+0.0006/year), July

(+0.0161/year) and September (+0.0081/year) but decreasing in August (-0.0025/year).

Therefore, heavy rainfall during monsoon season has also considerable increasing trend

(+0.0053/year) which means extreme weather is increasing.

12 y = 0.0366x - 66.459

R

2

= 0.0789

10

8

6

4

2

0

Fig. 7: Temporal variation of Heavy Rainfall of Bangladesh in Pre-monsoon Season during 1950-2010

6.5

6

5.5

5

4.5

4

3.5

y = 0.0053x - 5.5381

R

2

= 0.0356

3

Fig. 8: Temporal variation of Heavy Rainfall of Bangladesh in Monsoon Season during

1950-2010

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3.5 Example of extreme events:

a. Heavy Rainfall events in Dhaka on 14 August 2004 and 27 July 2009

Dhaka (city area) experienced 341 mm rainfall on 14 August 2004 and 333 mm rain on 27 July

2009 in 24 hours. Consequences of these heavy rainfalls are:

Most of the educational institutions were closed.

Life and business came to a halt.

Public transport services collapsed.

Slum dwellers lost most of their belongings.

Rain played havoc in the electricity supply creating power outage. b. Landslide on 11 June 2007 at Chittagong

Heavy rainfall resulted in a landslide in Chittagong, Bangladesh on 11 June 2007, killing 124 people and destroying houses, roads and embankments, as well as disrupting electricity, gas lines and communication facilities. According to the Bangladesh Meteorological Department

(BMD) rainfall measured on 11 June was 425 mm within 24 hours at Chittagong city area which is the heaviest in last 25 years.

3.6 Regional trends

It is well recognized in both the scientific and negotiating community that Bangladesh would be one of the most adversely affected countries to climate change. According to the Fourth

Assessment Report of WMO/UNEP Intergovernmental Panel on Climate Change (IPCC) released in 2007, the future projection of climate change indicates that south Asia is very likely to warm up during this century. Crop yields may decrease by 30% in the region by the mid-21 st century and considering the influence of population growth, the risk of hunger is projected to remain very high. Other predicted impacts of climate change include inundation of arable land, salinity intrusion, droughts, reduced fresh water, availability and persistence of transboundary pests and diseases.

3.7 Climate Change risks

All components of climate risk e.g. natural hazards and extreme weather events, impacts of climate change, exposure, vulnerabilities and low adaptive capacity all are visibly existent and seriously exposed because of highest density of population, their level of poverty, low adaptive capacity and natural resource dependent economy- particularly agriculture, considering all these Bangladesh will face enormous human sufferings in terms of food, water, shelter, health and overall livelihood maintenance unless proper measures are taken in time. Expansion and strengthening of capacity in generation and utilization of the emerging climate information and provision of effective early warning is the urgent need to support the Government and people for taking proper measure for sustainable environment and socio-economic development.

3.8 Government’s Climate Change Strategy and Action Plan: Climate change strategy and action plan of Bangladesh has been drawn on the four building blocks of the Bali Action Planadaptation to climate change, mitigation, technology transfer and adequate and timely flow of funds within a framework of food, energy, water and livelihoods security for all. It is a part of overall development strategy of the country. The climate change constraints and opportunities are being integrated into the overall development strategy of the country. The climate change

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constraints and opportunities are being integrated into the overall plan and programme involving all sectors. The National Climate Change Action Plan is built on the following six pillars: a. Food security, social protection and health to ensure that the poorest and most vulnerable in society including women and children, are protected from climate change and that all programmes focus on the needs of this group for food security, safe housing, employment and access to basic services including health. b. Comprehensive disaster management to further strengthen the countries already proven

Disaster Management System to deal with increasingly frequent and severe natural calamities. c. Infrastructure to ensure that existing assets (e.g. coastal and river embankments) are well maintained and fit for purpose and that urgently needed infrastructure (e.g. cyclone shelter and urban drainage) is put in place to deal with likely impacts of climate change. d. Research and knowledge management to predict the likely scale and timing of climate change impacts on different sectors of the economy and socio-economic groups to underpin future investment strategies; and to ensure that Bangladesh is a network into the latest global thinking on science and best practices of climate change management. e. Mitigation and low carbon development to evolve low carbon development options and implement these as the country’s economy grows over the coming decades and the demand for energy increases. f. Capacity building and institutional strengthening to enhance the capacity of Government ministries and agencies, civil society and the private sector to meet the challenge of climate change and mainstream them as a part of development action.

4. Measures taken for proper applications of weather and climate in disaster risk reduction and adaptation and mitigation of climate change:

Weather and climate information and an effective early warning system are the key elements for addressing climate change and reducing natural disaster risk.

4.1 Mandate of BMD

BMD is mandated to observe and monitor the weather and climate systems and issue of forecasts and warnings for all sorts of operations pertaining to Aviation, Maritime, Inland Water

Ways and advisories to the Disaster Management Bureau (DMB) and Relief Ministry in managing all types of natural disasters and its application in social and economic planning.

4. 2 Efforts for Disaster Risk Reduction

For disaster risk reduction the following are the four operation components for a successful of an end-to-end early warning system:

Generation of reliable and timely warnings

Quick and reliable dissemination to the targeted people and area

Good governance and all types of physical protections

 People’s sufficient awareness and perception about the content of the warning message and their resilient to sustain disaster.

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52500

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22500

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202500

195000

187500

180000

172500

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142500

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To execute the above perspectives, in the operation of an end-to-end early warning system the

Government has made paradigm shift in policy and governance by shifting from the concept of relief and rehabilitation to overall disaster risk management.

200000

150000

100000

50000

0

200000

138882

3363

Fig. 9: Causalities along with recorded cyclones in Bangladesh during 1970-2009

Fig. 10: Trend of reduction of causalities during similar intensity cyclones in

Bangladesh

Bangladesh has a long history of coping with major disasters. The Government of Bangladesh and people have a wealth of experience in preparing for, and responding to disaster events. In recent years, Bangladesh has been increasingly recognized as a leader in adopting a more holistic approach to risk reduction. During the last 38 years BMD has made significant improvement in cyclone forecasting and warnings as well as in the timely prediction of other severe weather phenomena, thereby contributing directly to the reduction of losses. The gradual reduction of death tolls for tropical cyclone is shown in figure below:

Fig. 11: Variation of GDP growth rate of Bangladesh under the influence of natural disasters.

4.3 Government initiatives for the improvement of Meteorological Service in Bangladesh

To contain the climate change impact, natural disaster risks and keeping environment for sustainable economic development, overall capacity enhancement of Bangladesh

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Meteorological Department (BMD) in the provision of effective early warning system for extreme events and proper climate services is extremely important. In the face of increasing extreme events and the vulnerability of climate change, demands for such accurate forecasts/warnings, more precise application of climate data and information based on local climate scenario development are increasing. Also, to maintain the food security and sustainable socioeconomic development, capacity for seasonal climate forecast for agriculture and climate scenario development in local perspective for proper adaptation and mitigation of climate change impact are very important for BMD.

For overall capacity enhancement of BMD in forecasting along with institutional up-gradation, the following initiatives are taken: a. Institutional up-gradation: Quality performance is the most important component for delivery of quality service. In terms of technological development, may initiatives have been undertaken at the moment to develop the infrastructural facilities and human capacity in BMD. But to uphold the efforts of sustainable development in the meteorological service, it is imperative that quality human resources be integrated with the system. For upholding BMD’s mandate in new perspective of climate change and disaster risk reduction efforts of Government, a proposal has been submitted to the

Government for induction of quality manpower along with institutional expansion for operation and maintenance of Numerical Weather Prediction (NWP), climate modeling, seasonal forecasting and more accurate and timely early warning system. b. Infrastructural development

BMD has taken many initiatives to modernize the existing weather and climate observatories, establishing new observatories, introduction of sophisticated Radar and

Communication Systems, capacity building for Numerical Weather Prediction (NWP)

System, downscaling capacity for climate modeling and up-gradation of storm-surge modeling system. As such the following projects have been taken during the last three years: a.

‘Improvement of Meteorological Radar System at Cox’s Bazar and Khepupara’ b. ‘Establishment of Meteorological Radar System at Moulvibazar’ c. ‘Establishment of 1 st Class Observatory at Five Places of Bangladesh [Panchagar

(Tetulia), Kishoregonj (Nikli), Khagrachari (Dighinala|), Cox’s Bazar (St. Martin) and

Bandarban]” d. ‘Up-gradation of Agro-meteorologiacl Services’ e. ‘Development of Human Capacity on Operation of Weather Analysis & Forecasting’ f. ‘Preparation of Wind Map of Coastal Areas/Feasible Areas of Bangladesh for Assessing

Power Generation Potential’ g. ‘Improvement & Relocation of Dhaka Meteorological Radar System for operation in aviation and Riverine Sectors and Protection of Urban System against National

Disasters’ h. ‘Numerical Weather Prediction System (2 nd Phase)’ i.

‘Up-gradation of 35 surface observatories through Establishment of Automatic

Meteorological Observing System & Wind Profilers’

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j. ‘Collaborating with International Centre for Theoretical Physics (ICTP), Italy, Beijing

Climate Centre (BCC), China and South Asian Climate Outlook Forum (SASCOF) k. Training programme on Storm Surge Modeling with expertise support from Japan

Meteorological Agency (JMA) and sponsored financially by Regional Integrated Multihazard Early Warning System (RIMES) has been arranged and in future we have a plan with WMO through Coastal Inundation Forecasting Demonstration Project (CIFDP) in

Bangladesh to integrate Storm Surge Model with Inundation Model to give local Specific surge height and inundation for taking better preparedness and local level. l. Global Framework for Climate Services (GFCS) is particularly meant for facilitation the

Governments in taking proper adaptation for the introduction of an end-to-end multisectoral service delivery system based on climate prediction utilizing national, regional and internationally collected weather and climate data. Furthermore, for effective utilization of GFCS opportunities, association with Regional Climate Centres (RCC’s) and Regional Climate Outlook Forum (RCOF) are important in achieving the national capacity to downscale and integrate those into the prediction system.

5. Conclusion

BMD is at present in a phase of transition; it is modernizing its observation and communication networks, changing the forecasting system from subjective to objective method and training its personnel to adapt to the ongoing change. But in the context of climate change BMD needs capacity enhancement urgently in the field of proper data management, downscaling capacity with data assimilation for global NWP products and climate model, tools of interaction to meet sectoral demands and strengthening the existing linkage with main stakeholders and users.

Furthermore, for effective utilization of GFCS opportunities, association with Regional Climate

Centres (RCC’s) and Regional Climate Outlook Forum (RCOF) are important, prior to achieve the national capacity to downscale and integrate those into prediction system. Bangladesh by virtue of its being an agro-based country, would be immensely benefited by accurate and reliable seasonal and multiple year long range prediction to guide farmers on the best cropping strategies and securities. The recent increase of Government association in the number of international agreements, declarations, conventions, related to weather, climate, water and related environmental issues requires more involvement of meteorological service. To make all the efforts fruitful, more international support and regional co-operation are required in terms of technology transfer, infrastructure development, capacity building and real time exchange of data and information which are quite indispensible for BMD.

Reference

Islam N. et al., 2008: ‘Understanding the rainfall climatology and detection of extreme weather events in SAARC region: Part I: Bangladesh’, SMRC Vol No. 21, SAARC Meteorological

Research Centre (SMRC), Dhaka, pp29-30.

Islam N. et al, 2008, Studies on summer monsoon rainfall using Regional Climate Model

PRECIS, SMRC Vol 22, p24.

Islam N. et al, 2008, Long-term Forecasting of Rainfall and Temperature in the SAARC region using RCM: Part I-Calibration, SMRC Vol. 30, p19.

Islam N. et al, 2009, Understanding the rainfall climatology and detection of extreme weather events in SAARC region: Part II-Bangladesh, SMRC Vol 29, p36.

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Islam N. and Das S., 2009: ‘Drought Diagnosis and Monitoring over Nepal and Bangladesh’,

Quamrul S. M. et al., 2008: ‘Study of sounding indices before severe thunderstorms

(Nor’westers)’ published in the ‘Proceedings of SAARC Seminar on ‘Norwester and

Tornadoes over SAARC Region and their Forecasting & Preparedness’, SAARC

Meteorological Research Centre (SMRC), Dhaka, pp10-18.

Islam N. and Mannan A., 2008: ‘Characteristics of Thunderstorms occur pre-monsoon period in

Bangladesh’ published in the ‘Proceedings of SAARC Seminar on ‘Nor’wester and

Tornadoes over SAARC Region and their Forecasti ng & Preparedness’, SAARC

Meteorological Research Centre (SMRC), Dhaka, pp86-93.

Mannan A. et al., 2008: ‘Heavy rainfall Activities in Monsoon Season and its Socio-economic impact in Bangladesh’ published in the ‘Proceedings of SAARC Seminar on ‘Application of Weather and Climate Forecasts in the Socio-economic Development and Disaster

Mitigation’, SAARC Meteorological Research Centre (SMRC), Dhaka, pp95-114.

Mannan A. et al., 2008: ‘Climatic feature of thunderstorm day and thunderstorm frequency and the ir impact on the society in Bangladesh’ published in the ‘Proceedings of SAARC

Seminar on ‘Application of Weather and Climate Forecasts in the Socio-economic

Development and Disaster Mitigation’, SAARC Meteorological Research Centre

(SMRC), Dhaka, pp11-26.

Mannan A. and Deeba F., 2008: ‘Variability of monsoon rainfall and its hydrological impact in

Bangladesh’ published in the Proceedings of SAARC Seminar on ‘Variability of southwest Monsoon and its Hydrological and Preparedness aspects over the SAARC

Reg ion’, SAARC Meteorological Research Centre (SMRC), Dhaka, pp67-74.

Mannan A. et al., 2008: ‘Correlation between Stability Indices derived from NCEP GDAS Data and thunderstorm occurrence in Bangladesh’ published in the ‘Proceedings of SAARC

Seminar on ‘Norwester and Tornadoes over SAARC Region and their Forecasting &

Preparedness’, SAARC Meteorological Research Centre (SMRC), Dhaka, pp51-60.

Mannan, A., 2010, Climate change and the behavior of cyclonic storm formed in the Bay of

Bengal and crossed Bangladesh Coast.

Quamrul S. M. et al., 2008: ‘Impact of Temperature Rise and Socio-economic Development of in Bangladesh’ published in the ‘Proceedings of SAARC Seminar on ‘Application of

Weather and Climate Forecasts in the Socio-economic Development and Disaster

Mitigation’, SAARC Meteorological Research Centre (SMRC), Dhaka, pp01-10.

SMRC Vol No. 26, SAARC Meteorological Research Centre (SMRC), Dhaka, pp44-45

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