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首页> 外文期刊>Sensors >Terrestrial Water Storage in African Hydrological Regimes Derived from GRACE Mission Data: Intercomparison of Spherical Harmonics, Mass Concentration, and Scalar Slepian Methods
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Terrestrial Water Storage in African Hydrological Regimes Derived from GRACE Mission Data: Intercomparison of Spherical Harmonics, Mass Concentration, and Scalar Slepian Methods

机译:从GRACE任务数据得出的非洲水文状况中的陆地水储量:球谐函数,质量浓度和标量Slepian方法的比较

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Spherical harmonics (SH) and mascon solutions are the two most common types of solutions for Gravity Recovery and Climate Experiment (GRACE) mass flux observations. However, SH signals are degraded by measurement and leakage errors. Mascon solutions (the Jet Propulsion Laboratory (JPL) release, herein) exhibit weakened signals at submascon resolutions. Both solutions require a scale factor examined by the CLM4.0 model to obtain the actual water storage signal. The Slepian localization method can avoid the SH leakage errors when applied to the basin scale. In this study, we estimate SH errors and scale factors for African hydrological regimes. Then, terrestrial water storage (TWS) in Africa is determined based on Slepian localization and compared with JPL-mascon and SH solutions. The three TWS estimates show good agreement for the TWS of large-sized and humid regimes but present discrepancies for the TWS of medium and small-sized regimes. Slepian localization is an effective method for deriving the TWS of arid zones. The TWS behavior in African regimes and its spatiotemporal variations are then examined. The negative TWS trends in the lower Nile and Sahara at ?1.08 and ?6.92 Gt/year, respectively, are higher than those previously reported.
机译:球谐(SH)和mascon解是重力恢复和气候实验(GRACE)质量通量观测的两种最常见的解决方案类型。但是,SH信号会因测量和泄漏误差而降低。 Mascon解决方案(此处为喷气推进实验室(JPL)版本)在亚Mascon分辨率下显示减弱的信号。两种解决方案都需要CLM4.0模型检查的比例因子,以获取实际的储水信号。当应用于盆地尺度时,Slepian定位方法可以避免SH泄漏误差。在这项研究中,我们估计了非洲水文系统的SH误差和比例因子。然后,根据Slepian定位确定非洲的地面水存储(TWS),并与JPL-mascon和SH解决方案进行比较。三台TWS的估算值与大型和潮湿地区的TWS吻合良好,但存在中小型地区的TWS差异。 Slepian本地化是推导干旱区TWS的有效方法。然后检查了非洲政权中的TWS行为及其时空变化。尼罗河下游和撒哈拉沙漠地区的TWS负趋势分别为每年1.08 Gt和6.92 Gt /年,高于先前报道的趋势。

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