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Description and evaluation of the Bergen climate model: ARPEGE coupled with MICOM

Bergen Open Research Archive

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dc.contributor.author Furevik, Tore en_US
dc.contributor.author Bentsen, Mats en_US
dc.contributor.author Drange, Helge en_US
dc.contributor.author Kindem, I. K. T. en_US
dc.contributor.author Kvamstø, Nils Gunnar en_US
dc.contributor.author Sorteberg, Asgeir en_US
dc.date.accessioned 2004-08-06T12:22:02Z en_US
dc.date.accessioned 2004-08-26T11:59:19Z
dc.date.available 2004-08-06T12:22:02Z en_US
dc.date.available 2004-08-26T11:59:19Z
dc.date.issued 2003-07 en_US
dc.identifier.citation Climate Dynamics 2003 21:27-51 en
dc.identifier.issn 1432-0894 en_US
dc.identifier.issn 0930-7575 en_US
dc.identifier.uri http://hdl.handle.net/1956/424
dc.identifier.uri http://dx.doi.org/10.1007/s00382-003-0317-5
dc.description.abstract A new coupled atmosphere–ocean–sea ice model has been developed, named the Bergen Climate Model (BCM). It consists of the atmospheric model ARPEGE/IFS, together with a global version of the ocean model MICOM including a dynamic–thermodynamic sea ice model. The coupling between the two models uses the OASIS software package. The new model concept is described, and results from a 300-year control integration is evaluated against observational data. In BCM, both the atmosphere and the ocean components use grids which can be irregular and have non-matching coastlines. Much effort has been put into the development of optimal interpolation schemes between the models, in particular the non-trivial problem of flux conservation in the coastal areas. A flux adjustment technique has been applied to the heat and fresh-water fluxes. There is, however, a weak drift in global mean sea-surface temperature (SST) and sea-surface salinity (SSS) of respectively 0.1 °C and 0.02 psu per century. The model gives a realistic simulation of the radiation balance at the top-of-the-atmosphere, and the net surface fluxes of longwave, shortwave, and turbulent heat fluxes are within observed values. Both global and total zonal means of cloud cover and precipitation are fairly close to observations, and errors are mainly related to the strength and positioning of the Hadley cell. The mean sea-level pressure (SLP) is well simulated, and both the mean state and the interannual standard deviation show realistic features. The SST field is several degrees too cold in the equatorial upwelling area in the Pacific, and about 1 °C too warm along the eastern margins of the oceans, and in the polar regions. The deviation from Levitus salinity is typically 0.1 psu – 0.4 psu, with a tendency for positive anomalies in the Northern Hemisphere, and negative in the Southern Hemisphere. The sea-ice distribution is realistic, but with too thin ice in the Arctic Ocean and too small ice coverage in the Southern Ocean. These model deficiencies have a strong influence on the surface air temperatures in these regions. Horizontal oceanic mass transports are in the lower range of those observed. The strength of the meridional overturning in the Atlantic is 18 Sv. An analysis of the large-scale variability in the model climate reveals realistic El Niño – Southern Oscillation (ENSO) and North Atlantic–Arctic Oscillation (NAO/AO) characteristics in the SLP and surface temperatures, including spatial patterns, frequencies, and strength. While the NAO/AO spectrum is white in SLP and red in temperature, the ENSO spectrum shows an energy maximum near 3 years. en_US
dc.format.extent 3257076 bytes en_US
dc.format.extent 93632 bytes
dc.format.extent 137 bytes
dc.format.extent 3257076 bytes
dc.format.mimetype application/pdf en_US
dc.format.mimetype text/plain
dc.format.mimetype text/plain
dc.format.mimetype application/pdf
dc.language.iso eng en_US
dc.publisher Springer en
dc.title Description and evaluation of the Bergen climate model: ARPEGE coupled with MICOM en_US
dc.type Journal article en
dc.type Peer reviewed en


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