Articles | Volume 12, issue 3
https://doi.org/10.5194/tc-12-811-2018
© Author(s) 2018. 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-12-811-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Modelling the climate and surface mass balance of polar ice sheets using RACMO2 – Part 1: Greenland (1958–2016)
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
Willem Jan van de Berg
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
J. Melchior van Wessem
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
Erik van Meijgaard
Royal Netherlands Meteorological Institute, De Bilt, the Netherlands
Dirk van As
Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark
Jan T. M. Lenaerts
Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, USA
Stef Lhermitte
Department of Geoscience & Remote Sensing, Delft University of Technology, Delft, the Netherlands
Peter Kuipers Munneke
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
C. J. P. Paul Smeets
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
Lambertus H. van Ulft
Royal Netherlands Meteorological Institute, De Bilt, the Netherlands
Roderik S. W. van de Wal
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
Michiel R. van den Broeke
Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands
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Latest update: 16 Aug 2024
Short summary
We present a detailed evaluation of the latest version of the regional climate model RACMO2.3p2 at 11 km resolution (1958–2016) over the Greenland ice sheet (GrIS). The model successfully reproduces the present-day climate and surface mass balance, i.e. snowfall minus meltwater run-off, of the GrIS compared to in situ observations. Since run-off from marginal narrow glaciers is poorly resolved at 11 km, further statistical downscaling to 1 km resolution is required for mass balance studies.
We present a detailed evaluation of the latest version of the regional climate model RACMO2.3p2...