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首页> 外文期刊>Journal of hydrometeorology >A Strong Linkage between Seasonal Crop Growth and Groundwater Storage Variability in India
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A Strong Linkage between Seasonal Crop Growth and Groundwater Storage Variability in India

机译:印度季节性作物生长与地下水储存变异性的强烈联系

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摘要

Groundwater is rapidly depleting in India primarily because of pumping for irrigation. However, the crucial role of crop growth at annual and seasonal time scales in groundwater storage variability remains mostly unexplored. Using the data from the Gravity Recovery Climate Experiment (GRACE) satellites and well observations, we show that crop growth is negatively correlated with groundwater storage at annual and seasonal time scales in north India. Precipitation is positively associated with groundwater storage variability at the yearly time scale in north-central India (NCI) and south India (SI). In contrast, precipitation is negatively correlated with groundwater storage from the GRACE satellites in northwest India (NWI). The negative correlation between precipitation and groundwater from the GRACE in NWI is primarily due to groundwater depletion due to anthropogenic pumping from deep aquifers. Precipitation and groundwater storage from the well observations are positively correlated in all the three regions, indicating the influence of precipitation on shallow aquifers. Analysis of the two main crop growing seasons (Rabi and Kharif) showed that crop growth is negatively related to groundwater storage in both Kharif (June-September) and Rabi seasons in north India (NWI and NCI). Groundwater contributes more than precipitation in NCI during the Kharif season and in NWI and SI during the Rabi season. Granger's causality test showed that groundwater is a significant contributor to crop growth in NWI and NCI in both Kharif and Rabi seasons. Our results highlight the need for agricultural water management in both the crop growing seasons in north India for reducing the rapid groundwater depletion.
机译:印度的地下水正在迅速枯竭,这主要是因为抽水灌溉。然而,作物生长在年度和季节时间尺度上对地下水储量变化的关键作用仍大部分未被探索。利用重力恢复气候实验(GRACE)卫星和油井观测的数据,我们表明,在印度北部的年度和季节时间尺度上,作物生长与地下水储量呈负相关。在印度中北部(NCI)和南部(SI)的年时间尺度上,降水量与地下水储量变化呈正相关。相比之下,降水量与印度西北部GRACE卫星(NWI)的地下水储量呈负相关。西北部GRACE地区的降水量与地下水之间的负相关主要是由于深层含水层的人为抽水导致地下水枯竭。这三个地区的降水量和井观测的地下水储量均呈正相关,表明降水对浅层含水层的影响。对两个主要作物生长季节(拉比和哈里夫)的分析表明,在哈里夫(6月至9月)和印度北部的拉比季节(NWI和NCI),作物生长与地下水储量呈负相关。在哈里夫季节,地下水对NCI的贡献大于降水,在拉比季节,地下水对NWI和SI的贡献大于降水。格兰杰因果关系检验表明,在哈里夫和拉比两个季节,地下水是NWI和NCI作物生长的重要贡献者。我们的研究结果强调了在印度北部作物生长季节进行农业用水管理的必要性,以减少地下水的快速枯竭。

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