Effects of winter and summer-time irrigation over Gangetic Plain on the mean and intra-seasonal variability of Indian summer monsoon

被引:0
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作者
Shubhi Agrawal
Arindam Chakraborty
Nirupam Karmakar
Simon Moulds
Ana Mijic
Wouter Buytaert
机构
[1] Indian Institute of Science,Centre for Atmospheric and Oceanic Sciences
[2] Indian Institute of Science,Divecha Centre for Climate Change
[3] University at Albany,Atmospheric Sciences Research Center
[4] State University of New York,Earth, Ocean and Atmospheric Science Department
[5] Florida State University,Centre for Water Systems
[6] University of Exeter,Department of Civil and Environmental Engineering
[7] Imperial College London,undefined
来源
Climate Dynamics | 2019年 / 53卷
关键词
Irrigation; Indian monsoon; Intraseasonal variability; North Atlantic Oscillations;
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中图分类号
学科分类号
摘要
The decreasing trend in rainfall in the last few decades over the Indo-Gangetic Plains of northern India as observed in ground-based observations puts increasing stress on groundwater because irrigation uses up to 70% of freshwater resources. In this work, we have analyzed the effects of extensive irrigation over the Gangetic Plains on the seasonal mean and intra-seasonal variability of the Indian summer monsoon, using a general circulation model and a very high-resolution soil moisture dataset created using extensive field observations in a state-of-the-art hydrological model. We find that the winter-time (November–March) irrigation has a positive feedback on the Indian summer monsoon through large scale circulation changes. These changes are analogous to a positive North Atlantic Oscillation (NAO) phase during winter months. The effects of the positive NAO phase persist from winter to spring through widespread changes in surface conditions over western and central Asia, which makes the pre-monsoon conditions suitable for a subsequent good monsoon over India. Winter-time irrigation also resulted in a reduction of low frequency intra-seasonal variability over the Indian region during the monsoon season. However, when irrigation is practiced throughout the year, a decrease in June–September precipitation over the Gangetic Plains, significant at 95% level, is noted as compared to the no-irrigation scenario. This decrease is attributed to the increase in local soil moisture due to irrigation, which results in a southward shift of the moisture convergence zone during the active phase of monsoon, decreasing its mean and intraseasonal variability. Interestingly, these changes show a remarkable similarity to the long-term trend in observed rainfall spatial pattern and low-frequency variability. Our results suggest that with a decline in the mean summer precipitation and stressed groundwater resources in the Gangetic Plains, the water crisis could exacerbate, with irrigation having a weakening effect on the regional monsoon.
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页码:3147 / 3166
页数:19
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