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229<br />
Wave estimations using winds from RCA, the Rossby regional climate<br />
model<br />
Barry Broman 1 and Ekaterini.E. Kriezi 2<br />
1 Swedish Meteorological and Hydrological Institute, Rossby Centre, Norrköping, Sweden; Barry.Broman@smhi.se<br />
2 Swedish Meteorological and Hydrological Institute, Göteborg, Sweden; Ekaterini.Kriezi@smhi.se<br />
1. Introduction<br />
Waves have now been used in the projections of the climate.<br />
The model SWAN running with winds from the Rossby<br />
Regional Climate Atmospheric model, (RCA). The first<br />
results of this were presented at the International<br />
Symposium US/EU-Baltic 2008 in Tallinn.<br />
2. Future Wave Climate<br />
Hind casts of waves were made with winds from RCA.<br />
When the results were compared to measurements they were<br />
to low. The reason is that the winds in RCA are too week<br />
due to among other thing averaging over the grid cell. In<br />
order to get better results a method were used to “correct”<br />
the winds by using both winds and gusts. This was a great<br />
improvement but more work is needed. In maps and graphs<br />
the comparisons will be given. Below in figure 1 you se an<br />
example of the climate effect on winds after taking the<br />
difference between a reference period and a future<br />
projection.<br />
Figure 1. example of results with the SWAN model<br />
(significant wave heights ): differences in percentiles<br />
between control period and future projection<br />
3. Future plans<br />
The plan is to use results from a coming coupled run<br />
between RCA, the atmospheric model and RCO the<br />
oceanographic model. These will give both winds and ice<br />
which is needed in order to make estimation of eventually<br />
changing wave climate in the Baltic<br />
References<br />
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from the regional climate model RCA of the Rossby<br />
Centre. US/EU-Baltic 2008, Tallinn may 27 -29 2008.