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Climate Change Impacts and Adaptation Assessment in Bangladesh

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Climate Change Impacts and Adaptation Assessment in Bangladesh
Vol. 12: 109–116, 1999

CLIMATE RESEARCH Clim Res

Published August 27

Climate change impacts and adaptation assessment in Bangladesh
Anwar Ali*
Space Research and Remote Sensing Organization (SPARRSO), Agargaon, Sher-e-Bangla Nagar, Dhaka 1207, Bangladesh

ABSTRACT: Bangladesh is likely to be one of the most vulnerable countries in the world to climate change. This paper discusses the possible impacts of climate change in Bangladesh through tropical cyclones, storm surges, coastal erosion and back water effect. The possible increase in cyclone frequency in the Bay of Bengal, lying south of Bangladesh, due to climate change is looked at by analyzing the cyclone data for 119 yr. Both qualitative and quantitative discussions are made on cyclone intensity increase for a sea surface temperature rise of 2 and 4°C. Different scenarios of storm surges under different climate change conditions are developed by using a numerical model of storm surges for the Bay of Bengal. Possible loss of land through beach erosion due to sea level rise on the eastern coast of Bangladesh is examined. Some discussions are also made on the impacts of back water effect due to sea level rise on flood situations in the country. Finally, a few remarks are made on the adaptation options for Bangladesh in the event of climate change. KEY WORDS: Bangladesh · Climate change · Impacts · Tropical cyclone · Storm surge · Erosion · Back water effect · Adaptations

1. INTRODUCTION Bangladesh is a disaster-prone country. Almost every year, the country experiences disasters of one kind or another — such as tropical cyclones, storm surges, coastal erosion, floods, and droughts — causing heavy loss of life and property and jeopardizing the development activities. The country is already beset with many problems like high population density (120 million people living in an area of 144 000 km2), shortage of land to accommodate the people, food security, human health, illiteracy, and so forth. The



Cited: Ali A (1980) Storm surges in the Bay of Bengal and their numerical modelling. SARC Tech Rep no. 120/80, Bangladesh Atomic Energy Commission, Dhaka Ali A (1995) Numerical investigation into the retardation of flood water outflow through the Meghna river in Bangladesh due to SW monsoon wind. Estuar Coast Shelf Sci 41:689–704 Ali A (1996) Vulnerability of Bangladesh to climate change and sea level rise through tropical cyclones and storm surges. J Water Air Soil Pollut 92d:171–179 Ali A, Chowdhury JU (1997) Tropical cyclone risk assessment with special reference to Bangladesh. MAUSAM (formerly Indian J Meteorol Hydrol Geophys) 48:305–322 Ali A, Rahman H, Chowdhury SSH, Begum QN (1997a) Back water effect of tides and storm surges on fresh water discharge through the Meghna estuary. J Remote Sensing Environ 1:85–95 Ali A, Rahman H, Chowdhury SSH (1997b) River discharge, storm surges and tidal interactions in the Meghna river mouth in Bangladesh. MAUSAM (formerly Indian J Meteorol Hydrol Geophys) 48:531–540 Bangladesh Climate Change Country Study Program (1997) Assessment of vulnerability and adaptation to climate change. Final report, Department of Environment, Govt of Bangladesh BCAS (1994) Vulnerability of Bangladesh to climate change and sea level rise: concepts and tools for calculating risk in integrated coastal zone management, Vols 1 & 2. Technical Report, Bangladesh Center for Advanced Studies, Dhaka Bruun P (1962) Sea level rise as a cause of shore erosion. J Waterways Harbors Div Proc Am Soc Civ Eng 88: 117–130 BUP (1994) Bangladesh: greenhouse effect and climate change. Briefing documents, Nos. 1–7, Bangladesh Unnayan Parishad (BUP), Dhaka, Bangladesh; Center for Environmental and Resource Studies (CEARS), University of Waikato, Hamilton; and Climate Research Institute, University of East Anglia, Norwich Emanuel KA (1987) The dependence of hurricane intensity. Nature 329:483–485 116 Clim Res 12: 109–116, 1999 Emanuel KA (1988) Toward a general theory of hurricanes. Am Sci 76:371–379 Frank WM (1985) Tropical cyclone formation. In: Elsberry RL (ed) Global view of tropical cyclones, based on the International Workshop on Tropical Cyclones, November 25–December 5, Bangkok, Thailand. US Office of Naval Research Marine Meteorological Program, p 53–90 Gray WM (1979) Hurricanes: their formation, structure and likely role in the tropical circulation. In: Shaw DB (ed) Meteorology over tropical oceans. Royal Meteorological Society, Bracknell, p 155–218 Hekstra GP (1989) Global warming and rising sea levels: the policy implications. The Ecologist 19:4–15 IMD (1979) Tracks of storms and depressions in the Bay of Bengal and the Arabian sea 1877–1970. India Meteorological Department (IMD), New Delhi Islam SMR, Huq S, Ali A (1999) Beach erosion in the eastern coastline of Bangladesh. In: Huq S, Karim Z, Asaduzzaman M, Mahtab F (eds) Vulnerability and adaption to climate change for Bangladesh. Kluwer Academic Publishers, Dordrecht, p 71–92 Mahtab F (1989) Effect of climate change and sea level rise on Bangladesh. Expert Group on climate change and sea level rise, Commonwealth Secretariat, London McBride JL (1995) Tropical cyclone formation. In: Elsberry RL (ed) Global perspectives on tropical cyclone. WMO Tech Doc WMO/TD-No. 693, Report No. TCP-38, WMO, Geneva, p 63–105 (reprinted 1996) MCSP (1992) Multipurpose cyclone shelter program. Final Report. Vol XI Special Studies, UNDP/World Bank/Govt of Bangladesh Project No. BGD/91/025 Miller BI (1958) On the maximum intensity of hurricanes. J Meteorol 15:184–195 Neumann CJ (1993) Global overview. Chapter 1, Global guide to tropical cyclone forecasting. WMO, Geneva Pramanik MAH (1983) Remote sensing applications to coastal morphological investigations in Bangladesh. PhD thesis, Jahangirnagar University, Savar, Dhaka Saunders MA, Harris AR (1997) Statistical evidence links exceptional 1995 Atlantic hurricane season to record sea warming. Geophys Res Lett 24:1255–1258 Wendland WM (1977) Tropical storm frequencies related to sea surface temperatures. J Appl Meteorol 6:477–481

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