Assessing the impacts of climate change on drought-prone regions in Bhima sub-basin (India) using the Standard Precipitation Index

被引:6
作者
Laddimath, Rajashekhar S. [1 ]
Patil, Nagraj S. [2 ]
Rao, P. S. [3 ]
Nagendra [2 ]
机构
[1] REVA Univ, Sch Civil Engn, Bengaluru, Karnataka, India
[2] Visvesvaraya Technol Univ, Ctr PG Studies, Dept Civil Engn, Belagavi, Karnataka, India
[3] Adv Ctr Integrated Water Resources Management ACI, Bengaluru, Karnataka, India
关键词
change factor method; climate change; extreme events; RCPs scenarios; spatio-temporal variation of drought; Standard Precipitation Index; KRISHNA BASIN; MODEL; UNCERTAINTIES; AGRICULTURE; TEMPERATURE; PROJECTIONS; RAINFALL; CHINA;
D O I
10.2166/wcc.2021.195
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
In Bhima sub-basin, the water sector is at high demand and in critical stress due to rapid urbanization. The past few decades witnessed extreme events and seasonal shifts due to anthropogenic activity triggered climate change. Thus, to evaluate the variability of extreme events, assessing the historical and future trends of precipitation in climate change scenarios is vital for making comprehensive mitigation and adaptation strategies. This paper examines the drought-prone regions by studying spatio-temporal variation of drought scenarios using the Standard Precipitation Index (SPI). Change factor method is used to downscale precipitation data from general circulation model (GCM) outputs under four Representative Concentration Pathway (RCP) scenarios to project future downscaled precipitation, to be input to examine the drought for 12 months. GCM and scenario uncertainty in climate change impact assessments are examined using box-whisker plots. Temporal variation for 12-month SPI shows significant changes over RCP scenarios. For the beginning of the period, 2021 precipitation is scanty for RCP 2.6 and 4.5 scenarios. Mild to moderate and severe drought events for the RCP 2.6 scenario are more predominant. Severe drought events under the RCP 6.0 scenario dominates over others. Lastly, the inconsistent pattern of drought events for RCP 8.5 is reported.
引用
收藏
页码:817 / 838
页数:22
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