Articles | Volume 11, issue 1
https://doi.org/10.5194/tc-11-427-2017
https://doi.org/10.5194/tc-11-427-2017
Research article
 | 
08 Feb 2017
Research article |  | 08 Feb 2017

Simultaneous disintegration of outlet glaciers in Porpoise Bay (Wilkes Land), East Antarctica, driven by sea ice break-up

Bertie W. J. Miles, Chris R. Stokes, and Stewart S. R. Jamieson

Viewed

Total article views: 3,989 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,007 1,806 176 3,989 132 164
  • HTML: 2,007
  • PDF: 1,806
  • XML: 176
  • Total: 3,989
  • BibTeX: 132
  • EndNote: 164
Views and downloads (calculated since 14 Jun 2016)
Cumulative views and downloads (calculated since 14 Jun 2016)

Cited

Latest update: 18 Apr 2024
Download
Short summary
We observe a large simultaneous calving event in Porpoise Bay, East Antarctica, where ~ 2900 km2 of ice was removed from floating glacier tongues between January and April 2007. This event was caused by the break-up of the multi-year sea ice usually occupies the bay, which we link to climatic forcing. We also observe a similar large calving event in March 2016 (~ 2200 km2), which we link to the long-term calving cycle of Holmes (West) Glacier.