Articles | Volume 14, issue 1
https://doi.org/10.5194/tc-14-261-2020
https://doi.org/10.5194/tc-14-261-2020
Research article
 | 
28 Jan 2020
Research article |  | 28 Jan 2020

Glacial sedimentation, fluxes and erosion rates associated with ice retreat in Petermann Fjord and Nares Strait, north-west Greenland

Kelly A. Hogan, Martin Jakobsson, Larry Mayer, Brendan T. Reilly, Anne E. Jennings, Joseph S. Stoner, Tove Nielsen, Katrine J. Andresen, Egon Nørmark, Katrien A. Heirman, Elina Kamla, Kevin Jerram, Christian Stranne, and Alan Mix

Viewed

Total article views: 3,233 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,028 1,123 82 3,233 335 80 94
  • HTML: 2,028
  • PDF: 1,123
  • XML: 82
  • Total: 3,233
  • Supplement: 335
  • BibTeX: 80
  • EndNote: 94
Views and downloads (calculated since 01 Aug 2019)
Cumulative views and downloads (calculated since 01 Aug 2019)

Viewed (geographical distribution)

Total article views: 3,233 (including HTML, PDF, and XML) Thereof 2,698 with geography defined and 535 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 27 Mar 2024
Download
Short summary
Glacial sediments in fjords hold a key record of environmental and ice dynamic changes during ice retreat. Here we use a comprehensive geophysical survey from the Petermann Fjord system in NW Greenland to map these sediments, identify depositional processes and calculate glacial erosion rates for the retreating palaeo-Petermann ice stream. Ice streaming is the dominant control on glacial erosion rates which vary by an order of magnitude during deglaciation and are in line with modern rates.