Articles | Volume 9, issue 5
https://doi.org/10.5194/tc-9-1773-2015
https://doi.org/10.5194/tc-9-1773-2015
Research article
 | 
08 Sep 2015
Research article |  | 08 Sep 2015

Evolution of Ossoue Glacier (French Pyrenees) since the end of the Little Ice Age

R. Marti, S. Gascoin, T. Houet, O. Ribière, D. Laffly, T. Condom, S. Monnier, M. Schmutz, C. Camerlynck, J. P. Tihay, J. M. Soubeyroux, and P. René

Viewed

Total article views: 6,271 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,136 2,811 324 6,271 397 197 193
  • HTML: 3,136
  • PDF: 2,811
  • XML: 324
  • Total: 6,271
  • Supplement: 397
  • BibTeX: 197
  • EndNote: 193
Views and downloads (calculated since 17 Apr 2015)
Cumulative views and downloads (calculated since 17 Apr 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 05 Nov 2024
Download
Short summary
Pyrenean glaciers are currently the southernmost glaciers in Europe. Using an exceptional archive of historical data sets and recent accurate observations, we propose the reconstruction of the length, area, elevation, and mass balance of Ossoue Glacier (French Pyrenees) since the Little Ice Age. We show that its evolution is in good agreement with climatic data. Assuming that the current ablation rate stays constant, Ossoue Glacier will disappear midway through the 21st century.