Articles | Volume 11, issue 3
https://doi.org/10.5194/tc-11-1501-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-11-1501-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
30 Jun 2017
Research article |
| 30 Jun 2017
Winter mass balance of Drangajökull ice cap (NW Iceland) derived from satellite sub-meter stereo images
Institute of Earth Sciences, University of Iceland, Askja,
Reykjavík, Iceland
Laboratoire d'Etudes en Géophysique et Océanographie
Spatiales, Centre National de la Recherche Scientifique (LEGOS–CNRS),
Université de Toulouse, Toulouse, France
Etienne Berthier
Laboratoire d'Etudes en Géophysique et Océanographie
Spatiales, Centre National de la Recherche Scientifique (LEGOS–CNRS),
Université de Toulouse, Toulouse, France
Eyjólfur Magnússon
Institute of Earth Sciences, University of Iceland, Askja,
Reykjavík, Iceland
Leif S. Anderson
Institute of Earth Sciences, University of Iceland, Askja,
Reykjavík, Iceland
Finnur Pálsson
Institute of Earth Sciences, University of Iceland, Askja,
Reykjavík, Iceland
Thorsteinn Thorsteinsson
Icelandic Meteorological Office, Reykjavík, Iceland
Ian M. Howat
School of Earth Sciences and Byrd Polar and Climate Research Center,
Ohio State University, Columbus, USA
Guðfinna Aðalgeirsdóttir
Institute of Earth Sciences, University of Iceland, Askja,
Reykjavík, Iceland
Tómas Jóhannesson
Icelandic Meteorological Office, Reykjavík, Iceland
Alexander H. Jarosch
Institute of Earth Sciences, University of Iceland, Askja,
Reykjavík, Iceland
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- Monitoring glacier albedo as a proxy to derive summer and annual surface mass balances from optical remote-sensing data L. Davaze et al. 10.5194/tc-12-271-2018
- Controls on the lifespans of Icelandic ice caps L. Anderson et al. 10.1016/j.epsl.2019.115780
- A scale-dependent model to represent changing aerodynamic roughness of ablating glacier ice based on repeat topographic surveys T. Smith et al. 10.1017/jog.2020.56
- Glaciohydrology of the Himalaya-Karakoram M. Azam et al. 10.1126/science.abf3668
- Uncertainty Analysis of Digital Elevation Models by Spatial Inference From Stable Terrain R. Hugonnet et al. 10.1109/JSTARS.2022.3188922
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- Mass balance, ice volume, and flow velocity of the Vestre Grønfjordbreen (Svalbard) from 2013/14 to 2019/20 A. Terekhov et al. 10.1080/15230430.2022.2150122
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- Evolution of geodetic mass balance over the largest lake-terminating glacier in the Tibetan Plateau with a revised radar penetration depth based on multi-source high-resolution satellite data Y. Zhou et al. 10.1016/j.rse.2022.113029
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- Volume Changes of Elbrus Glaciers From 1997 to 2017 S. Kutuzov et al. 10.3389/feart.2019.00153
- Correcting for Systematic Underestimation of Topographic Glacier Aerodynamic Roughness Values From Hintereisferner, Austria J. Chambers et al. 10.3389/feart.2021.691195
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Latest update: 18 Apr 2024
Short summary
Sub-meter satellite stereo images (Pléiades and WorldView2) are used to accurately measure snow accumulation and winter mass balance of Drangajökull ice cap. This is done by creating and comparing accurate digital elevation models. A glacier-wide geodetic mass balance of 3.33 ± 0.23 m w.e. is derived between October 2014 and May 2015. This method could be easily transposable to remote glaciated areas where seasonal mass balance measurements (especially winter accumulation) are lacking.
Sub-meter satellite stereo images (Pléiades and WorldView2) are used to accurately measure snow...
