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Water storage variations in the Poyang Lake Basin estimated from GRACE and satellite altimetry

机译:利用GRACE和卫星测高技术估算the阳湖流域的储水量变化

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摘要

The Gravity Recovery and Climate Experiment (GRACE) satellite mission provides a unique opportunity to quantitatively study terrestrial water storage (TWS) variations. In this paper, the terrestrial water storage variations in the Poyang Lake Basin are recovered from the GRACE gravity data from January 2003 to March 2014 and compared with the Global Land Data Assimilation System (GLDAS) hydrological models and satellite altimetry. Further-more, the impact of soil moisture content from GLDAS and rainfall from the Tropical Rainfall Measuring Mission (TRMM) on TWS variations are investigated. Our results indi-cate that the TWS variations from GRACE, GLDAS and satellite altimetry have a general consistency. The TWS trends in the Poyang Lake Basin determined from GRACE, GLDAS and satellite altimetry are increasing at 0.0141 km3/a, 0.0328 km3/a and 0.0238 km3/a, respectively during the investigated time period. The TWS is governed mainly by the soil moisture content and dominated primarily by the precipitation but also modulated by the flood season of the Yangtze River as well as the lake and river exchange water.
机译:重力恢复和气候实验(GRACE)卫星任务为定量研究陆地储水(TWS)的变化提供了独特的机会。本文从2003年1月至2014年3月的GRACE重力数据中恢复了the阳湖流域的地面水储量变化,并将其与全球土地数据同化系统(GLDAS)水文模型和卫星测高仪进行了比较。此外,还研究了来自GLDAS的土壤水分含量和来自热带降雨测量团(TRMM)的降雨对TWS变化的影响。我们的结果表明,来自GRACE,GLDAS和卫星测高仪的TWS变化具有总体一致性。由GRACE,GLDAS和卫星测高仪确定的the阳湖流域的TWS趋势在调查期间分别以0.0141 km3 / a,0.0328 km3 / a和0.0238 km3 / a的速度增长。 TWS主要由土壤水分含量控制,主要由降水决定,但也受长江洪灾季节以及湖泊和河流交换水的调节。

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  • 来源
    《大地测量与地球动力学(英文版)》 |2016年第2期|108-116|共9页
  • 作者单位

    School of Environment and Chemical Engineering, Shanghai University, Shanghai 200444, China;

    Shanghai Astronomical 0bservatory, Chinese Academy of Sciences, Shanghai 200030, China;

    School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China;

    School of Environment and Chemical Engineering, Shanghai University, Shanghai 200444, China;

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  • 入库时间 2022-08-19 03:54:06
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