HydroSat: geometric quantities of the global water cycle from geodetic satellites

被引:22
作者
Tourian, Mohammad J. [1 ]
Elmi, Omid [1 ]
Shafaghi, Yasin [2 ]
Behnia, Sajedeh [1 ]
Saemian, Peyman [1 ]
Schlesinger, Ron [1 ]
Sneeuw, Nico [1 ]
机构
[1] Univ Stuttgart, Inst Geodesy GIS, Stuttgart, Germany
[2] GAF AG, Munich, Germany
关键词
HIGH-TEMPORAL-RESOLUTION; LEVEL TIME-SERIES; SURFACE-WATER; RIVER DISCHARGE; ALTIMETRY; STORAGE; LAKES; RESERVOIRS; CALIBRATION; DYNAMICS;
D O I
10.5194/essd-14-2463-2022
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Against the backdrop of global change, in terms of both climate and demography, there is a pressing need for monitoring of the global water cycle. The publicly available global database is very limited in its spatial and temporal coverage worldwide. Moreover, the acquisition of in situ data and their delivery to the database have been in decline since the late 1970s, be it for economical or political reasons. Given the insufficient monitoring from in situ gauge networks, and with no outlook for improvement, spaceborne approaches have been under investigation for some years now. Satellite-based Earth observation with its global coverage and homogeneous accuracy has been demonstrated to be a potential alternative to in situ measurements. This paper presents HydroSat as a database containing geometric quantities of the global water cycle from geodetic satellites. HydroSat provides time series and their uncertainty in water level from satellite altimetry, surface water extent from satellite imagery, terrestrial water storage anomaly represented in equivalent water height from satellite gravimetry, lake and reservoir water volume anomaly from a combination of satellite altimetry and imagery, and river discharge from either satellite altimetry or imagery. The spatial and temporal coverage of these datasets varies and depends on the availability of geodetic satellites. These products, which are complementary to existing products, can contribute to our understanding of the global water cycle within the Earth system in several ways. They can be incorporated for hydrological modeling, they can be complementary to current and future spaceborne observations, and they can define indicators of the past and future state of the global freshwater system.
引用
收藏
页码:2463 / 2486
页数:24
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