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      Hydrological consistency using multi-sensor remote sensing data for water and energy cycle studies

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      Remote Sensing of Environment
      Elsevier BV

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          GRACE measurements of mass variability in the Earth system.

          Monthly gravity field estimates made by the twin Gravity Recovery and Climate Experiment (GRACE) satellites have a geoid height accuracy of 2 to 3 millimeters at a spatial resolution as small as 400 kilometers. The annual cycle in the geoid variations, up to 10 millimeters in some regions, peaked predominantly in the spring and fall seasons. Geoid variations observed over South America that can be largely attributed to surface water and groundwater changes show a clear separation between the large Amazon watershed and the smaller watersheds to the north. Such observations will help hydrologists to connect processes at traditional length scales (tens of kilometers or less) to those at regional and global scales.
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            The multi-institution North American Land Data Assimilation System (NLDAS): Utilizing multiple GCIP products and partners in a continental distributed hydrological modeling system

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              The North American Monsoon

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                Author and article information

                Journal
                Remote Sensing of Environment
                Remote Sensing of Environment
                Elsevier BV
                00344257
                February 2008
                February 2008
                : 112
                : 2
                : 430-444
                Article
                10.1016/j.rse.2007.03.027
                5a9b375b-a01c-4d55-aeae-058297ececbf
                © 2008

                http://www.elsevier.com/tdm/userlicense/1.0/

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