CORDIS Project
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This project aims to enhance understanding of glacier and ice sheet dynamics in a warming climate, focusing on the Antarctic Peninsula. It seeks to improve predictions of sea level rise by accurately modeling the loss of grounded ice due to ice shelf melting and collapse, particularly in the Larsen B Embayment region.
This project aims to improve our understanding of glacier and ice sheet dynamics in a warming climate, leading to a better forecast reliability for future sea level rise.
The main objective is to provide more accurate estimates for the loss of grounded ice in the Antarctic Peninsula, caused by the melting and collapse of its ice shelves over the last decades.
Increased losses of grounded ice have been observed at several places, in particular for the Larsen B Embayment glaciers which sped up and…
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