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• W3139596980 abstract "The Tibetan Plateau is located in central Asia with the highest mountain and extraordinary size, where geodynamic processes are very complex. The Glacial Isostatic Adjustment (GIA) effect in the Tibetan Plateau has been highly controversial because the past and present dimensions of ice sheets are suffering from large uncertainties. Larger differences in GIA estimates are found from different models or analyses based on the possible ice sheet and glacial history in Tibet. Present-day space geodetic techniques, such as Gravity Recovery and Climate Experiment (GRACE), are able to detect the vertical mass displacement and GIA uplift. In this paper, the GIA effects in the Tibetan Plateau are estimated and evaluated with GRACE" @default.
• W3139596980 created "2021-04-13" @default.
• W3139596980 creator A5008309018 @default.
• W3139596980 date "2013-01-01" @default.
• W3139596980 modified "2023-09-26" @default.
• W3139596980 title "Estimate of glacial isostatic adjustment uplift rate in the Tibetan Plateau from GRACE and GIA models" @default.
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