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首页> 外文期刊>Hydrology and Earth System Sciences >Identifying water mass depletion in northern Iraq observed by GRACE
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Identifying water mass depletion in northern Iraq observed by GRACE

机译:通过GRACE识别伊拉克北部的水质消耗

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Observations acquired by Gravity Recovery And Climate Experiment (GRACE) mission indicate a mass loss of 146 +/- 6 mm equivalent water height (EWH) in northern Iraq between 2007 and 2009. These data are used as an independent validation of lake mass variations and a rainfall-runoff model, which is based on local geology and climate conditions. Model inputs are precipitation from Tropical Rainfall Measurement Mission (TRMM) observations, and climatic parameters from Global Land Data Assimilation Systems (GLDAS) model parameters. The model is calibrated with observed river discharge and includes a representation of the karstified aquifers in the region to improve model realism. Lake mass variations were derived from Moderate Resolution Imaging Spectroradiometer (MODIS) in combination with satellite altimetry and some in situ data. Our rainfall-runoff model confirms that northern Iraq suffered a drought between 2007 and 2009 and captures the annual cycle and longer trend of the observed GRACE data. The total mass depletion seen by GRACE between 2007 and 2009 is mainly explained by a lake mass depletion of 75 +/- 3 mm EWH and a natural groundwater depletion of 39 +/- 8 mm EWH. Our findings indicate that anthropogenic groundwater extraction has a minor influence in this region, while a decline in lake mass and natural depletion of groundwater play a key role.
机译:重力恢复和气候实验(GRACE)任务获得的观测结果表明,2007年至2009年之间,伊拉克北部的水体质量损失为146 +/- 6毫米当量水高度(EWH)。这些数据被用作对湖体质量变化和基于当地地质和气候条件的降雨径流模型。模型输入是来自热带降雨测量任务(TRMM)观测的降水,以及来自全球土地数据同化系统(GLDAS)模型参数的气候参数。该模型已用观测到的河流流量进行了校准,并包含该地区岩溶化含水层的表示,以改善模型的真实性。湖泊质量变化是从中等分辨率成像光谱仪(MODIS)结合卫星测高仪和一些原位数据得出的。我们的降雨径流模型证实了伊拉克北部在2007年至2009年之间遭受干旱,并记录了观测到的GRACE数据的年度周期和更长的趋势。 GRACE在2007年至2009年间看到的总质量耗竭主要是由75 +/- 3 mm EWH的湖泊质量耗竭和39 +/- 8 mm EWH的天然地下水耗竭所解释的。我们的发现表明,人为提取地下水对该地区的影响较小,而湖泊水量的下降和地下水的自然枯竭则起着关键作用。

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