EGU22-5467
https://doi.org/10.5194/egusphere-egu22-5467
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Recent evolution of debris-covered glaciers in the Manaslu region of Nepal (1970 - 2019): the case of Ponkar Glacier

Adina E. Racoviteanu1,2, Neil F. Glasser3, Benjamin A. Robson4, Stephan Harrison1, Romain Millan2, Rijan B. Kayastha5, and Rakesh Kayastha5
Adina E. Racoviteanu et al.
  • 1Department of Geography, University of Exeter, United Kingdom (racovite@gmail.com)
  • 2Institut de Géosciences de l’Environnement, France
  • 3Department of Geography and Earth Sciences, Aberystwyth, United Kingdom of Great Britain – England, Scotland, Wales
  • 4Department of Earth Science, University of Bergen, Norway
  • 5Department of Environmental Science and Engineering, Kathmandu University, Nepal

Debris-covered glaciers in the Manaslu region of Nepal have been scarcely studied. Here we aim to fill this gap using new, multi-sensor, freely available 2019 Planet high-resolution (3 to 5 m) imagery, 1970 Corona declassified imagery and UAV and stake ablation data acquired in the field to characterize the surface and evolution of these glaciers over the last five decades. We report regional area changes, glacier thickness, geodetic glacier mass balance and surface velocity changes and focus on Ponkar Glacier and Thulagi Glacier and Lake for an in-depth assessment of surface geomorphology and surface feature dynamics (ponds, vegetation and ice cliffs).

Glaciers in the Manaslu region experienced a mean area loss of -0.26 ± 0.0001 % a-1 between 1970 and 2019, with a mean surface lowering of -0.20 ± 0.02 ma-1 over the period 1970 to 2013, corresponding to a regional geodetic mass balance of -0.17 ± 0.03 m w.e.a−1. Overall, debris-covered glaciers had higher thinning rates compared to clean ice glaciers. During the period 1970 to 2013, the debris-covered Ponkar Glacier had a geodetic mass balance of -0.06 ± 0.01 m w.e.a−1, with parts of the central trunk thickening and a nine-fold increase in the thinning rates over the lower parts of the glacier tongue in the recent years (2013 to 2019). Ice-surface morphology changes between 1970 and 2019 include a decrease in ogives and open crevasses, an increase in ice cliffs and ponds and the expansion of the supraglacial debris and ice-surface vegetation, suggesting reduced ice-dynamic activity.

How to cite: Racoviteanu, A. E., Glasser, N. F., Robson, B. A., Harrison, S., Millan, R., Kayastha, R. B., and Kayastha, R.: Recent evolution of debris-covered glaciers in the Manaslu region of Nepal (1970 - 2019): the case of Ponkar Glacier, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-5467, https://doi.org/10.5194/egusphere-egu22-5467, 2022.