Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica

East Antarctic ice shelves typically have cold ice cavities with low basal melt rates. Here the authors direct observational evidence of high basal melt rates beneath Shirase Glacier Tongue in East Antarctica, driven by inflowing warm water guided by a deep continuous trough extending to the contine...

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Autores principales:	Daisuke Hirano, Takeshi Tamura, Kazuya Kusahara, Kay I. Ohshima, Keith W. Nicholls, Shuki Ushio, Daisuke Simizu, Kazuya Ono, Masakazu Fujii, Yoshifumi Nogi, Shigeru Aoki
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/2458cc318d18427ca57280c4e9661776
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spelling	oai:doaj.org-article:2458cc318d18427ca57280c4e96617762021-12-02T19:02:28ZStrong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica10.1038/s41467-020-17527-42041-1723https://doaj.org/article/2458cc318d18427ca57280c4e96617762020-08-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-17527-4https://doaj.org/toc/2041-1723East Antarctic ice shelves typically have cold ice cavities with low basal melt rates. Here the authors direct observational evidence of high basal melt rates beneath Shirase Glacier Tongue in East Antarctica, driven by inflowing warm water guided by a deep continuous trough extending to the continental slope.Daisuke HiranoTakeshi TamuraKazuya KusaharaKay I. OhshimaKeith W. NichollsShuki UshioDaisuke SimizuKazuya OnoMasakazu FujiiYoshifumi NogiShigeru AokiNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-12 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Daisuke Hirano Takeshi Tamura Kazuya Kusahara Kay I. Ohshima Keith W. Nicholls Shuki Ushio Daisuke Simizu Kazuya Ono Masakazu Fujii Yoshifumi Nogi Shigeru Aoki Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica
description	East Antarctic ice shelves typically have cold ice cavities with low basal melt rates. Here the authors direct observational evidence of high basal melt rates beneath Shirase Glacier Tongue in East Antarctica, driven by inflowing warm water guided by a deep continuous trough extending to the continental slope.
format	article
author	Daisuke Hirano Takeshi Tamura Kazuya Kusahara Kay I. Ohshima Keith W. Nicholls Shuki Ushio Daisuke Simizu Kazuya Ono Masakazu Fujii Yoshifumi Nogi Shigeru Aoki
author_facet	Daisuke Hirano Takeshi Tamura Kazuya Kusahara Kay I. Ohshima Keith W. Nicholls Shuki Ushio Daisuke Simizu Kazuya Ono Masakazu Fujii Yoshifumi Nogi Shigeru Aoki
author_sort	Daisuke Hirano
title	Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica
title_short	Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica
title_full	Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica
title_fullStr	Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica
title_full_unstemmed	Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica
title_sort	strong ice-ocean interaction beneath shirase glacier tongue in east antarctica
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/2458cc318d18427ca57280c4e9661776
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Strong ice-ocean interaction beneath Shirase Glacier Tongue in East Antarctica

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