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How much groundwater did California's Central Valley lose during the 2012-2016 drought?

机译:加州的地下水在2012 - 2016年干旱期间减少了多少地下水?

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We estimate net groundwater storage change in the Central Valley from April 2002 to September 2016 as the difference between inflows and outflows, precipitation, evapotranspiration, and changes in soil moisture and surface water storage. We also estimate total water storage change attributable to groundwater change using Gravity Recovery and Climate Experiment (GRACE) satellite data, which should be equivalent to our water balance estimates. Over two drought periods within our 14-1/2years study period (January 2007 to December 2009 and October 2012 to September 2016), we estimate from our water balance that a total of 16.5km(3) and 40.0km(3) of groundwater was lost, respectively. Our water balance-based estimate of the overall groundwater loss over the 14-1/2years is -20.7km(3), which includes substantial recovery during nondrought periods The estimated rate of groundwater loss is greater during the recent drought (10.0 +/- 0.2 versus 5.5 +/- 0.3km(3)/yr) than in the 2007-2009 drought, due to lower net inflows, a transition from row crops to trees, and higher crop water use, notwithstanding a reduction in irrigated area. The GRACE estimates of groundwater loss (-5.0km(3)/yr for both water balance and GRACE during 2007-2009, and -11.2km(3)/yr for GRACE versus -10km(3)/yr for water balance during 2012-2016) are quite consistent for the two methods. However, over the entire study period, the GRACE-based groundwater loss estimate is almost triple that from the water balance, mostly because GRACE does not indicate the between-drought groundwater recovery that is inferred from our water balance.
机译:我们估计在中央谷地,从2002年4月2016年9月为土壤水分和地表蓄水的流入和流出,降水,蒸发,和变化之间的差异净地下水储量变化。我们也预计总蓄水变化归因于利用重力恢复和气候实验(GRACE)卫星数据地下水的变化,这应该是相当于我们的水平衡的估计。我们的14-1 /2年研究期间在两个干旱期(2007年1月至2009年12月和2012年10月至2016年9月),我们从我们的水平衡估计,共有地下水16.5公里(3)和40.0公里(3)丢了,分别。在14-1 /2年整体地下水损失的我们的水平衡为基础的估计是-20.7km(3),其中包括在nondrought期间地下水损失的估计速率是最近的干旱期间更大的大量回收(10.0 +/- 0.2与5.5 +/-0.3公里(3)/年)比在2007-2009干旱,适当降低净流入,从行作物树木的转变,并且提高了作物用水,尽管在灌溉面积的减少。地下水损失的GRACE估计(-5.0km(3)2007 - 2009年两个水平衡和GRACE /年,并-11.2km(3)在2012年为GRACE与水平衡-10km(3)/年/年-2016)是两种方法相当一致。然而,在整个研究期间,基于GRACE,地下水损耗估计近三倍,从水平衡,主要是因为GRACE并不表明是从我们的水平衡推断抗旱间地下水恢复。

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