Skip Navigation Links.
Collapse <span class="m110 colortj mt20 fontw700">Volume 12 (2024)</span>Volume 12 (2024)
Collapse <span class="m110 colortj mt20 fontw700">Volume 11 (2023)</span>Volume 11 (2023)
Collapse <span class="m110 colortj mt20 fontw700">Volume 10 (2022)</span>Volume 10 (2022)
Collapse <span class="m110 colortj mt20 fontw700">Volume 9 (2021)</span>Volume 9 (2021)
Collapse <span class="m110 colortj mt20 fontw700">Volume 8 (2020)</span>Volume 8 (2020)
Collapse <span class="m110 colortj mt20 fontw700">Volume 7 (2019)</span>Volume 7 (2019)
Collapse <span class="m110 colortj mt20 fontw700">Volume 6 (2018)</span>Volume 6 (2018)
Collapse <span class="m110 colortj mt20 fontw700">Volume 5 (2017)</span>Volume 5 (2017)
Collapse <span class="m110 colortj mt20 fontw700">Volume 4 (2016)</span>Volume 4 (2016)
Collapse <span class="m110 colortj mt20 fontw700">Volume 3 (2015)</span>Volume 3 (2015)
Collapse <span class="m110 colortj mt20 fontw700">Volume 2 (2014)</span>Volume 2 (2014)
Collapse <span class="m110 colortj mt20 fontw700">Volume 1 (2013)</span>Volume 1 (2013)
American Journal of Water Resources. 2019, 7(3), 95-105
DOI: 10.12691/AJWR-7-3-2
Original Research

Potential Changes to the Water Balance of the Teesta River Basin Due to Climate Change

Imran Khan1, and Dr. Mostafa Ali2

1River Engineering Division, Institute of Water Modelling, Dhaka, Bangladesh

2Water Resources Engineering Department, BUET, Dhaka, Bangladesh

Pub. Date: August 05, 2019

Cite this paper

Imran Khan and Dr. Mostafa Ali. Potential Changes to the Water Balance of the Teesta River Basin Due to Climate Change. American Journal of Water Resources. 2019; 7(3):95-105. doi: 10.12691/AJWR-7-3-2

Abstract

This study is carried out to assess the potential changes to the water balance of the Teesta River basin due to climate change. A semi-distributed hydrological model of Teesta river basin has been developed using SWAT (Soil Water Assessment Tool). After assessing the results of GCM solutions for 2080s, four scenarios has been selected for detail analysis. They are: Wettest, Driest, Warmest and Coolest. Among the selected scenarios, for the wettest scenario the precipitation had increased by 11.71% while it decreased by 1.76% for the driest scenario. The increase in temperature for the coolest and the warmest scenario is found to be 2.24¡ãC and 5.34¡ãC. The developed hydrological model of 1998-2013 timeframe served as the base model output to be compared against climate change model results. Comparing the water balance of the climate change model with the base model, it has been found that the monsoon season will become more wetter (as much as 48% increase of precipitation) and the dry season become more drier (as much as 43% reduction of precipitation) due to climate change for all the climate change scenarios. The flow comparison at the Dalia point, upstream of Teesta Barrage for different climate change scenarios shows similar kind of trend to that of the water balance comparison. The general trend emerging from the flow analysis is that the Dalia point will experience a more severe shortage of water during the lean season where, as much as 25% decrease of flow has been found even without any upstream controls.

Keywords

climate change, SWAT, water balance, Teesta river basin, Bangladesh

Copyright

Creative CommonsThis work is licensed under a Creative Commons Attribution 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

References

[1]  Prasai, S. and Mandakini D.S., Political economy Analysis of the Teesta River Basin, New Delhi: The Asia Foundation, March 2013. [Online] Available: https://asiafoundation.org/resources/pdfs/TheAsiaFoundation.Polit icalEconomyAnalysisoftheTeestaRiverBasin.March20131.pdf [Accessed May. 15, 2019].
 
[2]  Jaitley, A, ¡°South Asian perspectives on climate change and water policy¡±. In D. Michel & A. Pandya (Eds.), Troubled waters: Climate change, hydropolitics, and transboundary resources, The Henry L. Stimson Center, 2009. 17-32. [Online] Available: https://research.fit.edu/media/site-specific/researchfitedu/coast- climate-adaptation-library/africa/regional---africa/Michel-- Pandya.-2009.-Asia--Africa-Middle-East-Hydropolitics,- Transboundary-Resources--CC.pdf [Accessed May. 15, 2019].
 
[3]  Afroz, R and Rahman, M.A., ¡°Transboundary River Water for Ganges and Teesta Rivers in Bangladesh: An Assessment¡±. Global Science and Technology Journal, 1(1), 100-111.2013.
 
[4]  Centre for Inter Disciplinary Studies of Mountain and Hill Development (CISMHE), Carrying Capacity Study of Teesta Basin in Sikkim, University of Delhi, 2007. [Online] Available: http://www.actsikkim.com/docs/CCS_Executive_Summary.pdf. [Accessed May. 15, 2019].
 
[5]  Immerzeel, W. W., van Beek, L.P.H., and Bierkens, M.F.P., ¡°Climate Change Will Affect the Asian Water Towers¡±. Science, 328(5984), 1382-1385. 2010.
 
[6]  Strategic Foresight Group, Rivers of Peace, Mumbai: Strategic Foresight Group, 2013. 9-10. [Online] Available: https://www.strategicforesight.com/publication_pdf/22345riversof peace-website.pdf. [Accessed May. 15, 2019].
 
[7]  Mondal, S.H. and Islam, S., ¡°Chronological trends in maximum and minimum water flows of the Teesta River, Bangladesh, and its implications¡±. J¨¤mb¨¢: Journal of Disaster Risk Studies, 9(1), 373-384. 2017. [Online]Available: https://jamba.org.za/index.php/jamba/article/view/373/630 [Accessed May. 15, 2019].
 
[8]  Arnold, J. G. and Allen, P. M., ¡°Estimating hydrologic budgets for three Illinois watersheds¡±. Journal of Hydrology, 176 (1-4), 57¨C77. 1996.
 
[9]  Mengistu, D.T. and Sorteberg, A., ¡°Sensitivity of SWAT Simulated Streamflow to Climatic Changes within the Eastern Nile River Basin¡±. Hydrology and Earth System Sciences, 16, 391-407. 2012.
 
[10]  Williams, J.R., ¡°Flood routing with variable travel time or variable storage coefficients¡±. Trans. ASABE, 12(1), 100¨C103. 1969.