Atmospheric flow over Iceland has been simulated for the period January 1961 to July 2006, using the mesoscale MM5 model driven by initial and boundary data from the European Centre for Medium Range Weather Forecasts (ECMWF). Firstly, the simulated precipitation is compared to estimates derived from mass balance measurements on the Icelandic ice caps. It is found that the simulated precipitation compares favourably with the observed winter balance, in particular for Hofsjökull, where corrections to take liquid precipitation and/or winter ablation into account have been made, and for the outlet glaciers Dyngjujökull and Brúarjökull. Secondly, the model output is used as input to the WaSiM hydrological model to calculate and compare the runoff with observed runoff from six watersheds in Iceland. It is found that model results compare favourably with observations. Overall, the MM5 V3–7 is somewhat better than the MM5 V3–5. The V3–7 is drier than V3–5 on upstream slopes.
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Research Article|
April 01 2010
Dynamical downscaling of precipitation in Iceland 1961–2006
Ólafur Rögnvaldsson;
1Institute for Meteorological Research, Orkugarður, Grensásvegur 9, 108 Reykjavík, Iceland and Bergen School of Meteorology, Geophysical Institute, University of Bergen, Bergen, Norway
E-mail: [email protected]
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Jóna Finndís Jónsdóttir;
Jóna Finndís Jónsdóttir
2Formerly at the Hydrological Service, National Energy Authority, Reykjavík, Iceland
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Haraldur Ólafsson
Haraldur Ólafsson
3Faculty of Earth Sciences, University of Iceland, 101 Reykjavík, Iceland and Bergen School of Meteorology, Geophysical Institute, University of Bergen, Bergen, Norway
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Hydrology Research (2010) 41 (3-4): 153–163.
Article history
Received:
December 15 2008
Accepted:
January 04 2010
Citation
Ólafur Rögnvaldsson, Jóna Finndís Jónsdóttir, Haraldur Ólafsson; Dynamical downscaling of precipitation in Iceland 1961–2006. Hydrology Research 1 June 2010; 41 (3-4): 153–163. doi: https://doi.org/10.2166/nh.2010.132
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