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Autor:
Tim E. Van Peer, Osamu Seki, Oscar R. Romero, John P. Powell, Oliver Esper, Tina van de Flierdt, Laura De Santis, Shiv S. Singh, Justin D. Dodd, Amelia E. Shevenell, Molly P. Patterson, Benjamin K. Keisling, Giuseppe Cortese, François Beny, R. Mark Leckie, Jan Sverre Laberg, Jenny G. Gales, Saiko Sugisaki, Denise K. Kulhanek, Francesca Sangiorgi, Zhifang Xiong, David H. Harwood, Isabela M.Cordeiro De Sousa, Sookwan Kim, Wenshen Xiao, Saki Ishino, Sunghan Kim, Jeanine Ash, Juliane Müller, Robert M. McKay, Imogen B. Browne, Brian R. Romans
The marine-based West Antarctic Ice Sheet (WAIS) is currently retreating due to shifting wind-driven oceanic currents that transport warm waters toward the ice margin, resulting in ice shelf thinning and accelerated mass loss of the WAIS. Previous re
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5079907a37237941242dc80a5a73f3f
https://doi.org/10.14379/iodp.pr.374.2018
https://doi.org/10.14379/iodp.pr.374.2018
