Articles | Volume 12, issue 9
https://doi.org/10.5194/tc-12-3001-2018
https://doi.org/10.5194/tc-12-3001-2018
Research article
 | 
21 Sep 2018
Research article |  | 21 Sep 2018

Modelling the late Holocene and future evolution of Monacobreen, northern Spitsbergen

Johannes Oerlemans

Viewed

Total article views: 2,414 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,585 762 67 2,414 58 61
  • HTML: 1,585
  • PDF: 762
  • XML: 67
  • Total: 2,414
  • BibTeX: 58
  • EndNote: 61
Views and downloads (calculated since 16 Feb 2018)
Cumulative views and downloads (calculated since 16 Feb 2018)

Viewed (geographical distribution)

Total article views: 2,414 (including HTML, PDF, and XML) Thereof 2,157 with geography defined and 257 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Apr 2024
Download
Short summary
Monacobreen is a 40 km long surge-type tidewater glacier in northern Spitsbergen. The front is retreating fast. Calculations with a glacier model predict that due to future climate warming this glacier will have lost 20 to 40 % of its volume by the year 2100. Because of the glacier's memory, much of the response will come after 2100, even if the climatic conditions would stabilize.