The Cryosphere Discuss., 4, 561-602, 2010
www.the-cryosphere-discuss.net/4/561/2010/
doi:10.5194/tcd-4-561-2010
© Author(s) 2010. This work is distributed
under the Creative Commons Attribution 3.0 License.
Review Status
This discussion paper has been under review for the journal The Cryosphere (TC). Please refer to the corresponding final paper in TC.
Climate of the Greenland ice sheet using a high-resolution climate model – Part 1: Evaluation
J. Ettema1, M. R. van den Broeke1, E. van Meijgaard2, W. J. van de Berg1, J. E. Box3, and K. Steffen4
1Institute for Marine and Atmospheric research Utrecht, Utrecht University, Utrecht, The Netherlands
2Royal Netherlands Meteorological Institute, De Bilt, The Netherlands
3Department of Geography, Byrd Polar Research Center, Ohio State University, Columbia, Ohio, USA
4Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, Colorado, USA

Abstract. A simulation of 51 years (1957–2008) has been performed over Greenland using the regional atmospheric climate model RACMO2 at a horizontal grid spacing of 11 km forced by ECMWF analysis products. To better represent processes affecting ice sheet surface mass balance, such as melt water refreezing and penetration, an additional snow/ice surface module has been developed and implemented into the surface parameterisation of RACMO2v1. The temporal evolution and climatology of the model is evaluated with in situ coastal and ice sheet atmospheric measurements of near-surface variables and surface energy balance components. The bias for the near-surface air temperature (0.9 °C), specific humidity (0.1 g kg−1), wind speed (0.3 m s−1) as well as for radiative (2.5 W m−2 for net radiation) and turbulent heat fluxes shows that the model is in good accordance with available observations. The modeled surface energy budget underestimates the downward longwave radiation and overestimates the sensible heat flux. Due to their compensating effect, the averaged 2 m temperature bias is less than −0.9°C. The katabatic wind circulation is well captured by the model.

Citation: Ettema, J., van den Broeke, M. R., van Meijgaard, E., van de Berg, W. J., Box, J. E., and Steffen, K.: Climate of the Greenland ice sheet using a high-resolution climate model – Part 1: Evaluation, The Cryosphere Discuss., 4, 561-602, doi:10.5194/tcd-4-561-2010, 2010.
 
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