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Ice shelves are large floating ice masses, that are formed when glaciers are becoming afloat at the margin of ice sheets. One dominating mass loss mechanism of ice shelves is calving, describing the detachment of icebergs at the front. Ice shelves st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::596a1963f9636ee5b3ebeddbaf363f78
Autor:
Angelika Humbert, Veit Helm, Niklas Neckel, Ole Zeising, Martin Rückamp, Khan Shfaqat Abbas, Loebel Erik, Dietmar Gross, Rabea Sondershaus, Ralf Müller
The largest floating tongue of Greenland’s ice sheet, Nioghalvfjerdsbrae, has so far been relatively stable with respect to areal retreat. Curiously, it experienced significant less thinning and ice flow acceleration than its neighbour Zacharias Is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0be99a971583c4cf4d2cf6c8931c14eb
https://doi.org/10.5194/tc-2022-171
https://doi.org/10.5194/tc-2022-171