Impact of climate change on the hydrology of a semi-arid river basin of India under hypothetical and projected climate change scenarios

被引:11
|
作者
Desai, Sujeet [1 ]
Singh, D. K. [2 ]
Islam, Adlul [3 ,4 ]
Sarangi, A. [3 ]
机构
[1] ICAR Cent Coastal Agr Res Inst, Ella 403402, Goa, India
[2] ICAR Indian Agr Res Inst, Div Agr Engn, New Delhi 110012, India
[3] ICAR Indian Agr Res Inst, Water Technol Ctr, New Delhi 110012, India
[4] ICAR Res Complex, Nat Resource Management Div, Krishi Anusandhan Bhavan 2, New Delhi 110012, India
关键词
adaptation measures; climate change; evapotranspiration; MIROC5; surface runoff; SWAT; CMIP5 RCP SCENARIOS; WATER-RESOURCES; STREAMFLOW; EVAPOTRANSPIRATION; MODEL; SENSITIVITY; CROP; VARIABILITY; CO2;
D O I
10.2166/wcc.2020.287
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Climate change impact on the hydrology of the Betwa river basin, located in the semi-arid region of Central India, was assessed using the Soil and Water Assessment Tool (SWAT), driven by hypothetical scenarios and Model of Interdisciplinary Research on Climate version 5 (MIROC5) Global Circulation Model projections. SWAT-Calibration and Uncertainty Programs (SWAT-CUP) was used for calibration and validation of SWAT using multi-site streamflow data. The coefficient of determination, Nash-Sutcliffe efficiency, RMSE-observations standard deviation ratio and percent bias during calibration and validation period varied from 0.83-0.92, 0.6-0.91, 0.3-0.63 and -19.8-19.3, respectively. MIROC5 projections revealed an increase in annual mean temperature in the range of 0.7-0.9 degrees C, 1.2-2.0 degrees C and 1.1-3.1 degrees C during the 2020s, 2050s, and 2080s, respectively. Rainfall is likely to increase in the range of 0.4-9.1% and 5.7-15.3% during the 2050s and 2080s, respectively. Simulation results indicated 3.8-29% and 12-48% increase in mean annual surface runoff during the 2050s and 2080s, respectively. Similarly, an increase of 0.2-3.0%, 2.6-4.2% and 3.5-6.2% in mean annual evapotranspiration is likely during the 2020s, 2050s and 2080s, respectively. These results could be used for developing suitable climate change adaptation plans for the river basin.
引用
收藏
页码:969 / 996
页数:28
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