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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 2
Hydrol. Earth Syst. Sci., 15, 533–546, 2011
https://doi.org/10.5194/hess-15-533-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.
Hydrol. Earth Syst. Sci., 15, 533–546, 2011
https://doi.org/10.5194/hess-15-533-2011
© Author(s) 2011. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 09 Feb 2011

Research article | 09 Feb 2011

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

M. Becker1, B. Meyssignac1, L. Xavier1,2, A. Cazenave1, R. Alkama3, and B. Decharme3 M. Becker et al.
  • 1LEGOS/GOHS, UMR 5566/CNES/CNRS/UPS/IRD, Toulouse, France
  • 2COPPE/UFRJ, Rio de Janeiro, Brazil
  • 3Météo-France, CNRS, GAME, CNRM/GMGEC/UDC, Toulouse, France

Abstract. 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 Niño-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.

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