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Autor:
McKay, RM, De Santis, L, Kulhanek, DK, Ash, JA, Beny, F, Browne, IB, Cortese, G, De Sousa, IMC, Dodd, JD, Esper, OE, Gales, JG, Harwood, DH, Ishino, S, Keisling, BK, Kim, S, Laberg, JS, Leckie, RM, Müller, J, Patterson, MP, Romans, BR, Romero, OR, Sangiorgi, F, Seki, O, Powell, JP, Shevenell, A, Singh, SS, Sugisaki, S, Van De Flierdt, T, Van Peer, TE, Xiao, W, Xiong, Z
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=od______1032::ba3ee1aeb1a71fe3bc6aaadc7a0cf9b4
http://hdl.handle.net/10044/1/69291
http://hdl.handle.net/10044/1/69291