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Arctic winter climate and its interannual variations simulated by a regional climate model

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Citation:
Rinke, A. , Dethloff, K. and Christensen, J. H. (1999): Arctic winter climate and its interannual variations simulated by a regional climate model , Journal of Geophysical Research, 104 , pp. 19027-19038 .
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Abstract:

The mean Arctic January climatology and its interannual variation have been examined by simulations with aregional climate model of the Arctic atmosphere. To this end, an ensemble of monthlong simulations(January of the 11 years 1985-1995) has been investigated in which the ensemble is large enough to representa broad range of climatic conditions. The model produces credible simulations of the meteorological patterns.Only small deviations occur between simulations and European center for Medium-Range Weather Forecasts(ECMWF) analyses; that is, over most of the model area these differences in sea level pressure, 850 hPatemperature, and 500 hPa height are below 3 hPa, 1 K, and 5 m, respectively. Larger deviations (up to 5 hPa inthe sea level pressure and 20 m in the 500 hPa height) are found over parts of the Arctic Ocean, which seemsto be related to the crude sea ice representation at the lower model boundary and deficiencies in the planetaryboundary layer parameterization. It is shown that the dynamical aspects of the interannual variability can beadequately captured by the model simulations; that is, the maximum of the model bias of the dynamical variablesis significantly smaller than the interannual variability throughout the entire domain. To gain more insight into thespatial and temporal structures of the model's variability, an empirical orthogonal function (EOF) analysis hasbeen applied to determine the most significant structures in the fluctuations of the monthly mean dynamical fields.EOF 1 of the 500 hPa height field describes a regime with well-pronounced polar vortex and corresponds to the"Arctic Oscillation", whereas EOFs 2 and 3 show wave structures. A pronounced interannual variability is noticedin the time series of the amplitudes of the EOFs.

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