A physically based description of floodplain inundation dynamics in a global river routing model

Yamazaki, Dai G.; Kanae, Shinjiro; Kim, Hyungjun; Oki, Taikan

doi:10.1029/2010WR009726

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A physically based description of floodplain inundation dynamics in a global river routing model : FLOODPLAIN INUNDATION DYNAMICS

Author(s): Dai Yamazaki , Shinjiro Kanae , Hyungjun Kim , Taikan Oki

Publication date Created: April 2011

Publication date (Print): April 2011

Journal: Water Resources Research

Publisher: American Geophysical Union (AGU)

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GRACE measurements of mass variability in the Earth system.

Byron Tapley, Srinivas Bettadpur, John C. Ries … (2004)

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.