Articles | Volume 9, issue 5
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

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Cited articles

Berthier, E., Vincent, C., Magnusson, E., Gunnlaugsson, A. p., Pitte, P., Le Meur, E., Masiokas, M., Ruiz, L., Palsson, F., Belart, J. M. C., and Wagnon, P.: Glacier topography and elevation changes derived from Pleiades sub-meter stereo images, The Cryosphere, 8, 2275–2291., 2014.
Boé, J. and Habets, F.: Multi-decadal river flow variations in France, Hydrol. Earth Syst. Sci., 18, 691–708,, 2014.
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Büntgen, U., Frank, D., Grudd, H. K., and Esper, J.: Long-term summer temperature variations in the Pyrenees, Clim. Dynam., 31, 615–631, 2008.
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.