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Published byPhebe Hodge Modified over 9 years ago
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Coupled Climate Models OCEAN-ATMOSPHEREINTERACTIONS
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What is climate? n Different meanings –an external, forcing agent –influence on society and socio-economics –a background norm on which weather is imposed –temperature, rain, and humidity
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Climatic System 5 Major Components n Hydrosphere n Atmosphere n Cryosphere n Lithosphere n Biosphere
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Why does climate vary? VARIATIONS IN CLIMATE COMPONENTS
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Climate Forcings: the basis for change n Forcing: a change on the planetary energy balance system (flux) n 2 separate categories: –External Forcings –Internal Forcings n Human n Natural
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Climate Forcings: External n Milankovitch Cycles –Eccentricity –Obliquity –Precession n Solar Activity n Comet/meteorite impacts
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Climate Forcings: Internal Human induced n Greenhouse Gases n Tropospheric Aerosols n Ozone Depletion n Land Surface Changes KNOWN FORCINGS
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Climate Forcings: Internal Natural n Ocean circulation changes n Volcanic eruptions n Heat Transfer from interior
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Measurements that Drive the Models n Sea surface temperature n Air temperature and humidity n Wind velocity n Net radiation flux at ocean and underlying surfaces and upper atmospheric boundary n Fluxes of momentum, heat and moisture at the ocean-atmosphere boundary
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Coupled Climate Model n Combine oceanic and atmospheric models
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General Circulation Model: GCM n 3-dimensional model –scaling issues
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General Circulation Model: GCM n Solve for the main features of the atmosphere and ocean through a series of equations
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Atmospheric GCM
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AGCM variables n Surface Pressure n 2 horizontal wind components n Temperature n Moisture n Geopotential height
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AGCM: Physical Processes n Radiative Transfer –daily and annular cycles –short- and long-wave –clouds n Boundary Layer –friction –diurnal temperature and humidity variations
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AGCM: Physical Processes n Large-scale rainfall n Convection
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AGCM: Physical Processes n Land Surface Parameterization –gravity wave drag
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Oceanic GCM n Drivers –Winds –Salinity and density n Detailed schemes –Stronger currents on western sides of basin
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OGCMs n Swamp Model n Slab Model n Detailed Mixed Layer Model n Dynamic Ocean Model
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OGCM: Grid
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Other Schemes n Cyrosphere –hydrologic cycle –albedos n wind and heat n Vegetation –different scales –lack of validation data
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Coupled Model: AOGCM
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AOGCM Problems n Time Scales n Grid Scales n Costs
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AOGCM Solutions n Asynchronous Coupling
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Conclusion There is a long way to go before we have RELIABLE Models with which to predict CLIMATE and CLIMATE CHANGE …
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