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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- Holocene glacier and climate variations in Vestfirðir, Iceland, from the modeling of Drangajökull ice cap L. Anderson et al. 10.1016/j.quascirev.2018.04.024
- 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
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- 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
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- Uncertainty Assessment for Mean Snow Cover Depth Derived from Direct Measurements on Aldegondabreen Glacier (Svalbard) А. Terekhov et al. 10.31857/S2076673423030122
- The Utility of Optical Satellite Winter Snow Depths for Initializing a Glacio‐Hydrological Model of a High‐Elevation, Andean Catchment T. Shaw et al. 10.1029/2020WR027188
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- Beyond glacier-wide mass balances: parsing seasonal elevation change into spatially resolved patterns of accumulation and ablation at Wolverine Glacier, Alaska L. Zeller et al. 10.1017/jog.2022.46
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- Correcting for Systematic Underestimation of Topographic Glacier Aerodynamic Roughness Values From Hintereisferner, Austria J. Chambers et al. 10.3389/feart.2021.691195
- Evaluation of high‐resolution DEMs from satellite imagery for geomorphic applications: A case study using the SETSM algorithm A. Atwood & A. West 10.1002/esp.5263
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Latest update: 02 Nov 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...
