Articles | Volume 12, issue 2
https://doi.org/10.5194/tc-12-453-2018
https://doi.org/10.5194/tc-12-453-2018
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, Tore Hattermann, Susan L. Howard, and Laurie Padman

Viewed

Total article views: 4,212 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,832 1,265 115 4,212 667 119 138
  • HTML: 2,832
  • PDF: 1,265
  • XML: 115
  • Total: 4,212
  • Supplement: 667
  • BibTeX: 119
  • EndNote: 138
Views and downloads (calculated since 04 Aug 2017)
Cumulative views and downloads (calculated since 04 Aug 2017)

Viewed (geographical distribution)

Total article views: 4,212 (including HTML, PDF, and XML) Thereof 3,938 with geography defined and 274 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 14 Dec 2024
Download
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.