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Palma Massimiliano Iacono Roberto Sannino Gianmaria Bargagli Andrea Carillo Adriana Fekete Balazs M. Lombardi Emanuele Napolitano Ernesto Pisacane Giovanna Struglia Maria Vittoria 《Ocean Dynamics》2020,70(7):935-963
Ocean Dynamics - The tides in the Mediterranean Sea are generally weaker than in other regions of the world ocean, but are locally intensified in passages with complex bathymetry, such as the... 相似文献
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Vincenzo Artale Sandro Calmanti Adriana Carillo Alessandro Dell’Aquila Marine Herrmann Giovanna Pisacane Paolo M. Ruti Gianmaria Sannino Maria Vittoria Struglia Filippo Giorgi Xunqiang Bi Jeremy S. Pal Sara Rauscher 《Climate Dynamics》2010,35(5):721-740
We present an atmosphere–ocean regional climate model for the Mediterranean basin, called the PROTHEUS system, composed by the regional climate model RegCM3 as the atmospheric component and by a regional configuration of the MITgcm model as the oceanic component. The model is applied to an area encompassing the Mediterranean Sea and compared to a stand-alone version of its atmospheric component. An assessment of the model performances is done by using available observational datasets. Despite a persistent bias, the PROTHEUS system is able to capture the inter-annual variability of seasonal sea surface temperature (SST) and also the fine scale spatio-temporal evolution of observed SST anomalies, with spatial correlation as high as 0.7 during summer. The close inspection of a 10-day strong wind event during the summer of 2000 proves the capability of the PROTHEUS system to correctly describe the daily evolution of SST under strong air–sea interaction conditions. As a consequence of the model’s skill in reproducing observed SST and wind fields, we expect a reliable estimation of air–sea fluxes. The model skill in reproducing climatological land surface fields is in line with that of state of the art regional climate models. 相似文献
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