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Satellite-based estimates of groundwater depletion in India

机译:基于卫星的印度地下水消耗估算

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摘要

Groundwater is a primary source of fresh water in many parts of the world. Some regions are becoming overly dependent on it, consuming groundwater faster than it is naturally replenished and causing water tables to decline unremittingly. Indirect evidence suggests that this is the case in northwest India, but there has been no regional assessment of the rate of groundwater depletion. Here we use terrestrial water storage-change observations from the NASA Gravity Recovery and Climate Experiment satellites and simulated soil-water variations from a data-integrating hydrological modelling system to show that ground-water is being depleted at a mean rate of 4.0 ± 1.0 cm yr~(-1) equivalent height of water (17.7 ± 4.5km~3yr~(-1)) over the Indian states of Rajasthan, Punjab and Haryana (including Delhi). During our study period of August 2002 to October 2008, groundwater depletion was equivalent to a net loss of 109 km~3 of water, which is double the capacity of India's largest surface-water reservoir. Annual rainfall was close to normal throughout the period and we demonstrate that the other terrestrial water storage components (soil moisture, surface waters, snow, glaciers and biomass) did not contribute significantly to the observed decline in total water levels. Although our observational record is brief, the available evidence suggests that unsustainable consumption of groundwater for irrigation and other anthropogenic uses is likely to be the cause. If measures are not taken soon to ensure sustainable groundwater usage, the consequences for the 114,000,000 residents of the region may include a reduction of agricultural output and shortages of potable water, leading to extensive socio-economic stresses.
机译:在世界许多地区,地下水是淡水的主要来源。一些地区过度依赖地下水,消耗地下水的速度比自然补充的速度快,导致地下水位持续下降。间接证据表明,在印度西北部地区就是这种情况,但尚未对地下水枯竭率进行区域评估。在这里,我们使用来自NASA重力恢复和气候实验卫星的地面储水量变化观测数据,以及使用数据集成水文模型系统模拟的土壤水变化,显示地下水的平均消耗量为4.0±1.0 cm印度拉贾斯坦邦,旁遮普邦和哈里亚纳邦(包括德里)的yr〜(-1)水当量高度(17.7±4.5km〜3yr〜(-1))。在2002年8月至2008年10月的研究期间,地下水耗竭相当于净损失109 km〜3的水,是印度最大的地表水库的容量的两倍。在此期间,年降水量接近正常水平,我们证明了其他陆地储水成分(土壤水分,地表水,积雪,冰川和生物量)对观测到的总水位下降没有显着贡献。尽管我们的观察记录很简短,但现有证据表明,灌溉和其他人为用途的地下水消耗量不可持续,可能是原因。如果不尽快采取措施以确保地下水的可持续利用,那么对该地区1.14亿居民的后果可能包括农业产量减少和饮用水短缺,从而导致广泛的社会经济压力。

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  • 来源
    《Nature》 |2009年第7258期|999-1002|共4页
  • 作者单位

    Hydrological Sciences Branch, Code 614.3, NASA Goddard Space Flight Center, Greenbelt, Maryland 20771, USA;

    Department of Earth System Science, University of California, Irvine, California 92697-3100, USA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109-8099, USA Department of Physics, University of Udine, 208 Via delle Scienze, 33100 Udine, Italy;

    Department of Earth System Science, University of California, Irvine, California 92697-3100, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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