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Fifteen Years (1993–2007) of Surface Freshwater Storage Variability in the Ganges-Brahmaputra River Basin Using Multi-Satellite Observations

机译:恒河-布拉马普特拉河流域地表淡水储量变化的十五年(1993-2007),采用多卫星观测

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Surface water storage is a key component of the terrestrial hydrological and biogeochemical cycles that also plays a major role in water resources management. In this study, surface water storage (SWS) variations are estimated at monthly time-scale over 15 years (1993–2007) using a hypsographic approach based on the combination of topographic information from Advance Spaceborne Thermal Emission and Reflection Radiometer (ASTER) and Hydrological Modeling and Analysis Platform (HyMAP)-based Global Digital Elevation Models (GDEM) and the Global Inundation Extent Multi-Satellite (GIEMS) product in the Ganges-Brahmaputra basin. The monthly variations of the surface water storage are in good accordance with precipitation from Global Precipitation Climatology Project (GPCP), river discharges at the outlet of the Ganges and the Brahmaputra, and terrestrial water storage (TWS) from the Gravity Recovery And Climate Experiment (GRACE), with correlations higher than 0.85. Surface water storage presents a strong seasonal signal (~496 km 3 estimated by GIEMS/ASTER and ~378 km 3 by GIEMS/HyMAPs), representing ~51% and ~41% respectively of the total water storage signal and it exhibits a large inter-annual variability with strong negative anomalies during the drought-like conditions of 1994 or strong positive anomalies such as in 1998. This new dataset of SWS is a new, highly valuable source of information for hydrological and climate modeling studies of the Ganges-Brahmaputra river basin.
机译:地表水存储是陆地水文和生物地球化学循环的关键组成部分,在水资源管理中也起着重要作用。在这项研究中,基于超前星载热发射和反射辐射计(ASTER)的地形信息和水文信息的组合,采用潜航图方法,估计了15年内(1993-2007)每月时间尺度上的地表水储量(SWS)变化。恒河-布拉马普特拉盆地中基于建模和分析平台(HyMAP)的全球数字高程模型(GDEM)和全球淹没程度多卫星(GIEMS)产品。地表水储量的每月变化与全球降水气候学项目(GPCP)的降水量,恒河和雅鲁藏布特河口的河流排泄量以及重力恢复和气候实验(TWS)的地面水储量(TWS)完全相符( GRACE),相关系数高于0.85。地表水储量表现出强烈的季节性信号(由GIEMS / ASTER估算约为496 km 3,由GIEMS / HyMAPs估算约为〜378 km 3),分别占总储水信号的〜51%和〜41%,并表现出较大的变化。 -1994年干旱期间出现强负异常或1998年出现强正异常的年变化。SWS的这一新数据集为恒河-布拉马普特拉河的水文和气候模拟研究提供了新的,非常有价值的信息来源盆地。

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