Assessment of climate change impact on flow regimes over the Gomti River basin under IPCC AR5 climate change scenarios

被引:23
作者
Abeysingha, N. S. [1 ]
Islam, Adlul [2 ]
Singh, Man [3 ]
机构
[1] Rajarata Univ Sri Lanka, Dept Agr Engn & Soil Sci, Fac Agr, Anuradhapura, Sri Lanka
[2] Indian Council Agr Res, Nat Resource Management Div, New Delhi 110012, India
[3] Indian Agr Res Inst, Water Technol Ctr, New Delhi 110012, India
关键词
climate change; hybrid-delta method; sensitivity analysis; streamflow; SWAT-CUP; UNCERTAINTY ANALYSIS; CHANGE PROJECTIONS; WATER-RESOURCES; LAND-USE; DATA SET; SWAT; MODEL; STREAMFLOW; INDIA; EVAPOTRANSPIRATION;
D O I
10.2166/wcc.2018.039
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 flow regimes in the Gomti River basin, India was studied using the Soil and Water Assessment Tool (SWAT) driven by climate change scenarios generated from multiple general circulation model (GCM) projections. The SWAT-CUP (SWAT-Calibration and Uncertainty Programs) was used for calibration and validation of SWAT using multi-site data. Climate change scenarios were generated from multiple GCM projections using the hybrid-delta ensemble method. Calibration of SWAT using the nine most sensitive parameters showed that the model performed reasonably well with P-factor >0.7 and R-factor <1.0. The annual rainfall is projected to increase by 3.4-4.5, 4.7-10.0, and 5.0-18.0% during the 2020s, 2050s, and 2080s respectively under different Representative Concentration Pathways (RCPs). There is a decrease in rainfall during the winter season. The annual streamflow is projected to increase by 1-9, 1-22, and 2-38% during the 2020s, 2050s, and 2080s, respectively. However, winter and summer streamflow is projected to decrease. Magnitude and frequency of high flows is also projected to increase in the range of 3.6-27.3 and 12-87%, respectively under different RCPs. The results of this study will be helpful in developing suitable water management adaptation plans for the study basin.
引用
收藏
页码:303 / 326
页数:24
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