Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-3785-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-14-3785-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
06 Nov 2020
Research article |
| 06 Nov 2020
| 06 Nov 2020
The firn meltwater Retention Model Intercomparison Project (RetMIP): evaluation of nine firn models at four weather station sites on the Greenland ice sheet
Geological Survey of Denmark and Greenland, Copenhagen, Denmark
Department of Civil Engineering, Technical University of Denmark,
Kgs. Lyngby, Denmark
Ruth Mottram
Danish Meteorological Institute, Copenhagen, Denmark
Peter L. Langen
Department of Environmental Science, iClimate, Aarhus University, Roskilde, Denmark
Danish Meteorological Institute, Copenhagen, Denmark
Robert S. Fausto
Geological Survey of Denmark and Greenland, Copenhagen, Denmark
Martin Olesen
Danish Meteorological Institute, Copenhagen, Denmark
C. Max Stevens
Department of Earth and Space Sciences, University of Washington, Seattle, WA,
USA
Vincent Verjans
Lancaster Environment Centre, Lancaster University, Lancaster, UK
Amber Leeson
Lancaster Environment Centre, Lancaster University, Lancaster, UK
Stefan Ligtenberg
Institute for Marine and Atmospheric research, Utrecht University, Utrecht, the Netherlands
Weather Impact, Amersfoort, the Netherlands
Peter Kuipers Munneke
Institute for Marine and Atmospheric research, Utrecht University, Utrecht, the Netherlands
Sergey Marchenko
Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Ward van Pelt
Department of Earth Sciences, Uppsala University, Uppsala, Sweden
Colin R. Meyer
Thayer School of Engineering, Dartmouth College, Hanover, NH, USA
Sebastian B. Simonsen
National Space Institute, Technical University of Denmark, Kgs.
Lyngby, Denmark
Achim Heilig
Department of Earth and Environmental Sciences, Ludwig Maximilian University, Munich, Germany
Samira Samimi
Department of Geography, University of Calgary, Calgary, AB, Canada
Shawn Marshall
Department of Geography, University of Calgary, Calgary, AB, Canada
Horst Machguth
Department of Geosciences, University of Fribourg, Fribourg, Switzerland
Michael MacFerrin
Cooperative Institute for Research in Environmental Sciences,
University of Colorado, Boulder, CO, USA
Masashi Niwano
Meteorological Research Institute, Japan Meteorological Agency,
Tsukuba, 305-0052 Japan
Olivia Miller
US Geological Survey, Utah Water Science Center, Salt Lake City,
UT, USA
Clifford I. Voss
US Geological Survey, Menlo Park, CA, USA
Jason E. Box
Geological Survey of Denmark and Greenland, Copenhagen, Denmark
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- Hydrologic modeling of a perennial firn aquifer in southeast Greenland O. Miller et al. 10.1017/jog.2022.88
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- Time‐Domain Reflectometry Measurements and Modeling of Firn Meltwater Infiltration at DYE‐2, Greenland S. Samimi et al. 10.1029/2021JF006295
- Spatial Response of Greenland's Firn Layer to NAO Variability M. Brils et al. 10.1029/2023JF007082
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- Firn changes at Colle Gnifetti revealed with a high-resolution process-based physical model approach E. Mattea et al. 10.5194/tc-15-3181-2021
- Recent warming trends of the Greenland ice sheet documented by historical firn and ice temperature observations and machine learning B. Vandecrux et al. 10.5194/tc-18-609-2024
- Firn on ice sheets C. Amory et al. 10.1038/s43017-023-00507-9
- The singing firn J. Chaput et al. 10.1017/aog.2023.34
- Uncertainty in East Antarctic Firn Thickness Constrained Using a Model Ensemble Approach V. Verjans et al. 10.1029/2020GL092060
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- A new Level 4 multi-sensor ice surface temperature product for the Greenland Ice Sheet I. Karagali et al. 10.5194/tc-16-3703-2022
- Antarctic-wide ice-shelf firn emulation reveals robust future firn air depletion signal for the Antarctic Peninsula D. Dunmire et al. 10.1038/s43247-024-01255-4
- Review article: Melt-affected ice cores for polar research in a warming world D. Moser et al. 10.5194/tc-18-2691-2024
- Programme for Monitoring of the Greenland Ice Sheet (PROMICE) automatic weather station data R. Fausto et al. 10.5194/essd-13-3819-2021
- Quantifying Antarctic‐Wide Ice‐Shelf Surface Melt Volume Using Microwave and Firn Model Data: 1980 to 2021 A. Banwell et al. 10.1029/2023GL102744
- Ice Sheet Surface and Subsurface Melt Water Discrimination Using Multi‐Frequency Microwave Radiometry A. Colliander et al. 10.1029/2021GL096599
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- The Greenland Firn Compaction Verification and Reconnaissance (FirnCover) dataset, 2013–2019 M. MacFerrin et al. 10.5194/essd-14-955-2022
- Spatial characterization of near-surface structure and meltwater runoff conditions across the Devon Ice Cap from dual-frequency radar reflectivity K. Chan et al. 10.5194/tc-17-1839-2023
- Improved representation of the contemporary Greenland ice sheet firn layer by IMAU-FDM v1.2G M. Brils et al. 10.5194/gmd-15-7121-2022
- The Determination of the Snow Optical Grain Diameter and Snowmelt Area on the Greenland Ice Sheet Using Spaceborne Optical Observations B. Vandecrux et al. 10.3390/rs14040932
- Large interannual variability in supraglacial lakes around East Antarctica J. Arthur et al. 10.1038/s41467-022-29385-3
- Study on the Ablation of the Glacier Covered by Mineral Dust in Alpine Regions Z. Zhang et al. 10.3390/w14131982
- In situ measurements of meltwater flow through snow and firn in the accumulation zone of the SW Greenland Ice Sheet N. Clerx et al. 10.5194/tc-16-4379-2022
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Latest update: 01 Nov 2024
Short summary
In the vast interior of the Greenland ice sheet, snow accumulates into a thick and porous layer called firn. Each summer, the firn retains part of the meltwater generated at the surface and buffers sea-level rise. In this study, we compare nine firn models traditionally used to quantify this retention at four sites and evaluate their performance against a set of in situ observations. We highlight limitations of certain model designs and give perspectives for future model development.
In the vast interior of the Greenland ice sheet, snow accumulates into a thick and porous layer...
