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Groundwater storage change detection from in situ and GRACE-based estimates in major river basins across India

机译:印度主要河流盆地原位和基于恩典估计的地下水储存变更检测

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摘要

India has been the subject of many recent groundwater studies due to the rapid depletion of groundwater in large parts of the country. However, few if any of these studies have examined groundwater storage conditions in all of India's river basins individually. Herein we assess groundwater storage changes in all 22 of India's major river basins using in situ data from 3420 observation locations for the period 2003-2014. One-month and 12-month standardized precipitation index measures (SPI-1 and SPI-12) indicate fluctuations in the long-term pattern. The Ganges and Brahmaputra basins experienced long-term decreasing trends in precipitation in both 1961-2014 and the study period, 2003-2014. Indeterminate or increasing precipitation trends occurred in other basins. Satellite-based and in situ groundwater storage time series exhibited similar patterns, with increases in most of the basins. However, diminishing groundwater storage (at rates of 0.4 km(3)/year) was revealed in the Ganges-Brahmaputra River Basin based on in situ observations, which is particularly important due to its agricultural productivity.
机译:由于该国大部分地下水迅速消耗地下水迅速,印度一直是最近的地下水研究的主题。然而,很少有这些研究在印度所有的河流盆地中检测了地下水储存条件。在此,我们在2003 - 2014年期间的3420个观察位置的原位数据中评估了印度所有主要河流盆地的地下水储存变化。一个月和12个月的标准化降水指数措施(SPI-1和SPI-12)表示长期模式的波动。恒河和Brahmaputra盆地在1961 - 2014年和研究期间经历了长期降水趋势,2003 - 2014年。其他盆地发生不确定或增加降水趋势。基于卫星和原位地下水储存时间序列表现出类似的模式,大部分盆地增加。然而,基于原位观察的Ganges-Brahmaputra河流域揭示了地下水储存(以> 0.4公里(3)/年的速度),这是由于其农业生产率尤为重要。

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