Articles | Volume 14, issue 7
https://doi.org/10.5194/tc-14-2205-2020
https://doi.org/10.5194/tc-14-2205-2020
Research article
 | 
13 Jul 2020
Research article |  | 13 Jul 2020

Impact of West Antarctic ice shelf melting on Southern Ocean hydrography

Yoshihiro Nakayama, Ralph Timmermann, and Hartmut H. Hellmer

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (16 Apr 2020) by Petra Heil
AR by Yoshihiro Nakayama on behalf of the Authors (30 Apr 2020)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (29 May 2020) by Petra Heil
AR by Yoshihiro Nakayama on behalf of the Authors (31 May 2020)  Author's response    Manuscript
ED: Publish subject to technical corrections (11 Jun 2020) by Petra Heil
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Short summary
Previous studies have shown accelerations of West Antarctic glaciers, implying that basal melt rates of these glaciers were small and increased in the middle of the 20th century. We conduct coupled sea ice–ice shelf–ocean simulations with different levels of ice shelf melting from West Antarctic glaciers. This study reveals how far and how quickly glacial meltwater from ice shelves in the Amundsen and Bellingshausen seas propagates downstream into the Ross Sea and along the East Antarctic coast.