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Past terrestrial water storage (1980–2008) in the Amazon Basin reconstructed from GRACE and in situ river gauging data

机译:过去的亚马逊盆地(1980-2008)从恩典和原位河河衡量数据重建

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Terrestrial water storage (TWS) composed of surface waters, soil moisture, groundwater and snow where appropriate, is a key element of global and continental water cycle. Since 2002, the Gravity Recovery and Climate Experiment (GRACE) space gravimetry mission provides a new tool to measure large-scale TWS variations. However, for the past few decades, direct estimate of TWS variability is accessible from hydrological modeling only. Here we propose a novel approach that combines GRACE-based TWS spatial patterns with multi-decadal-long in situ river level records, to reconstruct past 2-D TWS over a river basin. Results are presented for the Amazon Basin for the period 1980–2008, focusing on the interannual time scale. Results are compared with past TWS estimated by the global hydrological model ISBA-TRIP. Correlations between reconstructed past interannual TWS variability and known climate forcing modes over the region (e.g., El Ni?o-Southern Oscillation and Pacific Decadal Oscillation) are also estimated. This method offers new perspective for improving our knowledge of past interannual TWS in world river basins where natural climate variability (as opposed to direct anthropogenic forcing) drives TWS variations.
机译:陆地储水(TWS)由表面水域,土壤水分,地下水和雪组成,是全球和大陆水循环的关键要素。自2002年以来,重力恢复和气候实验(Grace)空间重量计量使命提供了一种测量大规模TWS变化的新工具。但是,在过去的几十年里,只能从水文建模访问TWS变异性的直接估计。在这里,我们提出了一种新颖的方法,将基于Grace的TWS空间模式结合在于多层河流河水位记录,以重建过去的河流盆地的二进制。 1980 - 2008年期间的亚马逊盆地提出了结果,重点是持续时间尺度。结果与全球水文模型估计的过去的TWS进行了比较。还估计了在该地区(例如,EL NI?O-Southern振荡和太平洋振荡和太平洋横向振荡)之间重建的过去续际TWS变异性和已知的气候迫使模式之间的相关性。该方法提供了新的视角,可提高我们对世界河流盆地过去际TWS的知识,其中天然气气候变异性(与直接人为强制)驱动TWS变异。

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