Climate of the Past
Climate of the Past
CP
Articles | Volume 19, issue 7
Articles | Volume 19, issue 7
https://doi.org/10.5194/cp-19-1321-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-19-1321-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 7
Research article
 | 
10 Jul 2023
Research article |  | 10 Jul 2023

A High Arctic inner shelf–fjord system from the Last Glacial Maximum to the present: Bessel Fjord and southwest Dove Bugt, northeastern Greenland

Kevin Zoller, Jan Sverre Laberg, Tom Arne Rydningen, Katrine Husum, and Matthias Forwick

Viewed

Total article views: 1,295 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
954 280 61 1,295 44 51
  • HTML: 954
  • PDF: 280
  • XML: 61
  • Total: 1,295
  • BibTeX: 44
  • EndNote: 51
Views and downloads (calculated since 11 Oct 2022)
Cumulative views and downloads (calculated since 11 Oct 2022)

Viewed (geographical distribution)

Total article views: 1,295 (including HTML, PDF, and XML) Thereof 1,222 with geography defined and 73 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 17 Nov 2024
Download
Short summary
Marine geologic data from NE Greenland provide new information about the behavior of the Greenland Ice Sheet from the last glacial period to present. Seafloor landforms suggest that a large, fast-flowing ice stream moved south through southern Dove Bugt. This region is believed to have been deglaciated from at least 11.4 ka cal BP. Ice in an adjacent fjord, Bessel Fjord, may have retreated to its modern position by 7.1 ka cal BP, and the ice halted or readvanced multiple times upon deglaciation.
Read more