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185<br />

An atmosphere-ocean regional climate model for the Mediterranean area:<br />

Present climate and XXI scenario simulations<br />

V. Artale, S. Calmanti, A. Carillo, A. Dell’Aquila, M. Herrmann, G. Pisacane, PM Ruti * and<br />

G. Sannino, MV Struglia<br />

ACS/CLIM-MOD, ENEA, Roma, Italy; paolo.ruti@enea.it<br />

F. Giorgi, X. Bi, J.S. Pal and S. Rauscher<br />

Abdus Salam ICTP,Trieste, Italy<br />

In the framework of CIRCE EU Project, an atmosphereocean<br />

regional climate model (AORCM) for the<br />

Mediterranean basin, called the PROTHEUS system, is<br />

presented. The PROTHEUS system is composed of the<br />

regional climate model RegCM3 as atmospheric component<br />

and a regional configuration of the MITgcm model as<br />

oceanic component.<br />

The model is applied to an area encompassing the<br />

Mediterranean Sea and the adjacent basin (Fig. 1), where the<br />

fine scale feedbacks associated with air-sea interactions can<br />

substantially influence the spatial and temporal structure of<br />

regional climate. We compare a 40-year simulation with the<br />

PROTHEUS system driven by ERA40 reanalysis fields at<br />

the lateral boundaries with a corresponding simulation<br />

performed with the stand-alone configuration of the<br />

atmospheric model RegCM3. We show that the coupled<br />

system produces realistic features of atmospheric<br />

circulations, land surface climate, ocean sea surface<br />

temperature (SST), ocean surface circulations and air-sea<br />

fluxes.<br />

The main improvement associated with the use of the<br />

coupled system is found by considering the high spatiotemporal<br />

variability of surface fields. First, the coupled<br />

model is able to capture the fine scale spatio-temporal<br />

evolution of observed SST. Second, large changes in air-sea<br />

fluxes are associated to the changes in SST and yield a better<br />

simulation of fine temporal scale climate variability. Given<br />

the successful development of the coupled model system<br />

here described we envisage a number of possible<br />

applications of the PROTHEUS system.<br />

In this perspective, we have also performed a 1951-2050<br />

scenario simulation driven by ECHAM5-MPIOM fields at<br />

the lateral boundaries. Preliminary results from this run are<br />

here shown.<br />

Figure 1. Domain for: a) RegCM and b) MITgcm<br />

with corresponding topography. Units are m.

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