Zobrazeno 1 - 4
of 4
pro vyhledávání: '"H. L. Seroussi"'
Publikováno v:
The Cryosphere, Vol 16, Pp 451-469 (2022)
Increasing melt of ice sheets at their floating or vertical interfaces with the ocean is a major driver of marine ice sheet retreat and sea level rise. However, the extent to which warm, salty seawater may drive melting under the grounded portions of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d0cab58553a7968deb0272fc36d84222
https://tc.copernicus.org/preprints/tc-2021-262/
https://tc.copernicus.org/preprints/tc-2021-262/
Publikováno v:
Geophysical Research Letters. 48
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8be29f93615c32adfaad0b8b8f8439aa
https://doi.org/10.1029/2021gl093213
https://doi.org/10.1029/2021gl093213
Autor:
David G. Vaughan, Andrew M. Hilger, Riley Culberg, Dustin M. Schroeder, Winnie C.W. Chu, Thomas M. Jordan, Duncan A. Young, H. L. Seroussi, Donald D. Blankenship
Publikováno v:
Journal of geophysical research. Earth surface. 126(10)
The Amundsen Sea Embayment of the West Antarctic Ice Sheet contains Thwaites and Pine Island Glaciers, two of the most rapidly changing glaciers in Antarctica. To date, Pine Island and Thwaites Glaciers have only been observed by independent airborne
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f0ebd70747859de69f5e860e25dce96e
https://pubmed.ncbi.nlm.nih.gov/35865452
https://pubmed.ncbi.nlm.nih.gov/35865452
Publikováno v:
Geophysical research letters. 48(18):e2021
Satellite-based estimates of ice shelf melt rates reach similar to 200 m yr-1 close to the grounding line of Pine Island Glacier, in West Antarctica. However, ocean simulations have not yet been able to reproduce such high melt rates, even with high-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c19c9d098a9c04636fbd4aef16e34e1b
http://hdl.handle.net/2115/84616
http://hdl.handle.net/2115/84616