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The Glacial Isostatic Adjustment (GIA) effect in the Tibetan Plateau has been controversial because the past and present dimensions of ice sheets are not clear and in-situ observations are less. In this study, the Gravity Recovery And Climate Experiment (GRACE) and Ice, Cloud, and land Elevation Satellite (ICESat) measurements are used to estimate the ice mass balance and Glacier Isostatic Adjustment...
The Gravity Recovery and Climate Experiment (GRACE) and the Ice, Cloud, and land Elevation Satellite (ICESat) missions can estimate the ice mass changes in Greenland. The GRACE monthly time-varying gravity filed solution can be used to infer the redistribution of temporal redistribution with a limited spatial resolution of 300–500 km, while the ICESat measurements can estimate the elevation variations...
Continental ice sheets are frozen from fresh-water with volume change related to temperature, snowfall, river runoff and evapotranspiration, which affect and are affected by changes in Earth's climate. The ice sheets variations play an important role in global water cycle and understanding land and ocean water exchange and energy balance. However, it is very difficult to accurately monitor the continental...
Terrestrial water storage (TWS) is an important parameter in water resource manages and research of land-surface processes and hydrological cycle. However, the traditional instruments are very difficult to monitor global high temporal-spatial terrestrial water storage and its variability without a comprehensive global monitoring network of hydrological parameters due to high cost and high labor intensity...
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