Articles | Volume 12, issue 2
The Cryosphere, 12, 453–476, 2018
The Cryosphere, 12, 453–476, 2018

Research article 06 Feb 2018

Research article | 06 Feb 2018

Tidal influences on a future evolution of the Filchner–Ronne Ice Shelf cavity in the Weddell Sea, Antarctica

Rachael D. Mueller et al.


Interactive discussion

Status: closed
Status: closed
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
AR by Svenja Lange on behalf of the Authors (22 Nov 2017)  Author's response
ED: Publish as is (27 Nov 2017) by G. Hilmar Gudmundsson
Short summary
There is evidence that climate change in the Weddell Sea will cause warmer water to flow toward the icy continent and into the ocean cavity circulating beneath a thick (~ 1000 m) ice sheet extension that floats over the Weddell Sea, called the Filchner–Ronne Ice Shelf (FRIS). This paper addresses the impact of this potential warming on the melting of FRIS. It evaluates the previously unexplored feedbacks between ice melting, changes in cavity geometry, tides, and circulation.