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Modelling the Atmospheric, Oceanic and Coupled System

  • Brian Hoskins
  • Paul S. Schopf
  • Antonio Navarra
Conference paper
Part of the NATO Science Series book series (NAIV, volume 82)

A model of the coupled system consists of component models of the atmosphere and of the ocean as well as software to link the two. The atmosphere must see the slowly evolving ocean sea surface temperature (SST) while the ocean must see the rapidly changing weather, in the form of the surface exchange of momentum, heat and freshwater. Although one should consider the coupled system as a whole, much progress has been made by considering aspects of the atmosphere and ocean modules separately. Computer restrictions mean that both the atmospheric and oceanic components have to be simplified. Many processes in both media take place at scales smaller than can be resolved by the component models and so must be parameterised as they cannot be explicitly resolved. Methods to deal with limitations to parameterisation are discussed. A variety of ways of validating testing and improving atmospheric general circulation models is considered.

Keywords

Couple Model Couple System Ocean Model Atmospheric Model Potential Vorticity 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer Science + Business Media B.V 2008

Authors and Affiliations

  • Brian Hoskins
    • 1
  • Paul S. Schopf
    • 2
  • Antonio Navarra
    • 3
  1. 1.Department of MeteorologyUniversity of ReadingEarley GateUK
  2. 2.Department of Climate Dynamics, College of ScienceGeorge Mason UniversityFairfaxUSA
  3. 3.Istituto Nazionale di Geofisica e VulcanologiaCentro Euro-Mediterraneo per I Cambiamenti ClimaticiItaly

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