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ESSD | Articles | Volume 12, issue 2
Earth Syst. Sci. Data, 12, 887–896, 2020
https://doi.org/10.5194/essd-12-887-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Earth Syst. Sci. Data, 12, 887–896, 2020
https://doi.org/10.5194/essd-12-887-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Data description paper 20 Apr 2020

Data description paper | 20 Apr 2020

An updated seabed bathymetry beneath Larsen C Ice Shelf, Antarctic Peninsula

Alex Brisbourne et al.

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Status: closed
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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Alex Brisbourne on behalf of the Authors (03 Mar 2020)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (06 Mar 2020) by Giuseppe M.R. Manzella
AR by Alex Brisbourne on behalf of the Authors (11 Mar 2020)  Author's response    Manuscript
ED: Publish as is (18 Mar 2020) by Giuseppe M.R. Manzella
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Short summary
Melting of the Larsen C Ice Shelf in Antarctica may lead to its collapse. To help estimate its lifespan we need to understand how the ocean can circulate beneath. This requires knowledge of the geometry of the sub-shelf cavity. New and existing measurements of seabed depth are integrated to produce a map of the ocean cavity beneath the ice shelf. The observed deep seabed may provide a pathway for circulation of warm ocean water but at the same time reduce rapid tidal melt at a critical location.
Melting of the Larsen C Ice Shelf in Antarctica may lead to its collapse. To help estimate its...
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