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  • 1
    Publication Date: 2017-04-04
    Description: In this study, two numerical simulations of the 20th Century climate performed with two global GCM are analysed, with the ultimate goal of isolating the impact of oceanic mesoscale features on the climate of the euro- mediterranean region, and its interannual variability. In the first experiment (L), a T159 atmosphere (equivalent to ∼80 Km horizontal resolution) is coupled to a 2x2- degree global ocean model, with a locally enhanced 0.5-degree resolution over the Mediterranean Sea region. In the second experiment (H), the same T159 atmosphere is coupled to a global ocean model regional high-resolution 1/16-degree (∼7 Km) ocean model for the Mediterranea Sea, which is connected to a low-resolution OGCM for the global ocean (identical to the ocean model used in L) . Thus, in H, as far as the Mediterranean area is concerned, the atmosphere is coupled to an ocean model which resolves mesoscale features (“turbulent” ocean), whereas in L the atmosphere interacts with a more “laminar” oceanic system. Since these two experiments are identical except for the resolution of the ocean model over the Mediterranean Sea , the systematic comparison of H and L will allow the assessment of the net effects on the climate of the Euro-Mediterranean region from explicitly resolving mesoscale oceanic features in the coupled model.
    Description: Unpublished
    Description: Zurich
    Description: 3.7. Dinamica del clima e dell'oceano
    Description: open
    Keywords: Mediterranean Sea ; eddies ; climate ; 01. Atmosphere::01.01. Atmosphere::01.01.02. Climate
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2017-04-04
    Description: Within the CIRCE (Climate Change and Impact Research: The Mediterranean Environment) EU Project, substantial efforts were devoted to enhance the representation of the oceanic system in the Mediterranean region. This was achieved by developing coupled general circulation models with ocean components which either explicitly resolve, or simply permit, mesoscale circulation features. The inclusion of the eddy variability tail in the spectrum of the processes resolved by the modelled system represents a particularly relevant step forward with respect to the previous CMIP3 generation of climate models , as these were systematically based on coarse resolution ocean components, leading in turn to an extremely rough representation of the Mediterranean Sea sub-system. In this study the role of mesoscale oceanic features on the air-sea interactions over the Mediterranean region was analysed, in the context of one of the CIRCE ensemble of climate models. To this aim, two different simulations of the 20th Century climate, performed with two distinct configurations of the CMCC coupled general circulation model featuring radically different horizontal resolutions in the Mediterranean Sea domain, were compared. This comparison highlights the implications deriving from the inclusion of energetic ocean mesoscale structures in the variability spectrum of the coupled ocean-atmosphere system and points to the need for high-resolution ocean components in the development of next generation climate model.
    Description: Unpublished
    Description: Wien, Austria
    Description: 3.7. Dinamica del clima e dell'oceano
    Description: open
    Keywords: mediterranean Sea ; eddies ; climate models ; 01. Atmosphere::01.01. Atmosphere::01.01.02. Climate
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
    Location Call Number Limitation Availability
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