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Basin-scale water-balance estimates of terrestrial water storage variations from ECMWF operational forecast analysis

机译:ECMWF运行预报分析得出的流域规模水平衡估算

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摘要

In recent publications, a new basin-scale dataset of monthly variations in terrestrial water storage (BSWB) was derived for the ERA40 time period (1958-2002) using an atmospheric-terrestrial water-balance approach (Seneviratne et al., 2004; Hirschi et al., 2006). Here, we test the feasibility of using ECMWF operational forecast analyses available for the recent time period in near real time instead of reanalysis data for the derivation of these estimates. Our results suggest that the moisture flux convergence from the ECMWF operational forecast analysis is generally consistent with ERA40 in the investigated regions, including 35 mid-latitude river basins and domains. For ten domains with recent streamflow measurements, water-balance estimates of monthly terrestrial water storage variations derived using the ECMWF operational forecast data are compared with estimates from the Gravity Recovery and Climate Experiment (GRACE). In general the atmospheric-terrestrial water-balance estimates show more geographical detail than the analyzed standard resolution GRACE products.
机译:在最近的出版物中,使用大气-地面水平衡方法(Seneviratne等,2004; Hirschi)得出了ERA40时间段(1958-2002)的地面水储量(BSWB)月度变化的新流域规模数据集。等人,2006)。在这里,我们测试了近实时使用ECMWF操作预测分析的可行性,而不是使用重新分析数据来估算这些估计值。我们的结果表明,来自ECMWF运行预测分析的水分通量收敛在所调查的地区(包括35个中纬度河流域和地区)总体上与ERA40一致。对于最近进行流量测量的十个域,将使用ECMWF运行预测数据得出的每月地面水储量变化的水平衡估计值与重力恢复和气候实验(GRACE)的估计值进行比较。通常,与分析的标准分辨率GRACE产品相比,大气-陆地水平衡估计值显示更多的地理细节。

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