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GLDAS_NOAH_M.2.1水文模型在青藏高原的适定性分析
引用本文:钱安,易爽,孙广通,王秋玲,苏占东.GLDAS_NOAH_M.2.1水文模型在青藏高原的适定性分析[J].大地测量与地球动力学,2018,38(3):254-259.
作者姓名:钱安  易爽  孙广通  王秋玲  苏占东
作者单位:防灾科技学院防灾工程系;北海道大学理学研究院;
摘    要:利用2003-01~2016-06共162个月 GLDAS_NOAH_M.2.1、GLDAS_NOAH_M.001新旧水文模型和GRACE卫星重力数据,计算青藏高原区域水储量及总质量变化,说明GLDAS_NOAH_M.2.1水文模型相对于旧模型可提升在青藏高原区域的精度。将研究区域分为6个部分,根据3种数据分别计算6个区域的平均质量变化时间序列,顾及年周期、半年周期对该时间序列进行最小二乘拟合,估计6个区域3种数据的年振幅、年相位及相关性。结果表明,GLDAS_NOAH_M.2.1水储量变化的年振幅、年相位与GRACE总质量变化的年振幅、年相位空间分布大体一致,在青藏高原北部区域与GRACE的相关性尤为明显;GLDAS_NOAH_M.001年振幅、年相位在青藏高原北部区域存在明显异常,与GRACE的相关性很低。从长趋势质量变化来看, GLDAS新、旧模型在不同区域的差异为-6.4~4.5 Gt/a量级,而在青藏高原主体区域,新模型的质量趋势偏低10.4 Gt/a。


GLDAS_NOAH_M.2.1 Hydrological Model and Its Application Analysis in the Qinghai-Tibet Plateau
QIAN An,YI Shuang,SUN Guangtong,WANG Qiuling,SU Zhandong.GLDAS_NOAH_M.2.1 Hydrological Model and Its Application Analysis in the Qinghai-Tibet Plateau[J].Journal of Geodesy and Geodynamics,2018,38(3):254-259.
Authors:QIAN An  YI Shuang  SUN Guangtong  WANG Qiuling  SU Zhandong
Abstract:A new GLDAS_NOAH_M.2.1 land water model and its old version of GLDAS_NOAH_M.001 from January 2003 and June 2016, totally 162 months, are investigated here with GRACE satellite gravimetry observations to study soil moisture and total mass change in the Qinghai-Tibet plateau. Our result shows that GLDAS_NOAH_M.2.1 has an improved precision in simulating soil moisture change. Here, 6 study regions are divided and in each region these three data sets are used to estimate mass changes, whose correlation coefficient and periodic terms are derived. Compared with GLDAS_NOAH_M.001, GLDAS_NOAH_M.2.1 has a better performance in correlation with GRACE in terms of periodic variations. The correlation between GLDAS_NOAH_M.001 and GRACE is very poor in northern Tibet, while GLDAS_NOAH_M.2.1 has improved this condition. In terms of secular mass change, GLDAS_NOAH_M.2.1 brings a difference at the order of -6.4~4.5 Gt/a in different regions and a total different of -10.4 Gt/a in the main part of Qinghai-Tibet plateau.
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