Definition
An AOGCM refers to a 3D numerical model which solves the central conservation equations, e.g., mass, momentum, and energy, to derive the characteristic global-scale fluid dynamical flow (the “general circulation”) as well as temperature of a planetary atmosphere and ocean. The atmosphere and ocean modules are coupled via surface exchange fluxes of energy (e.g., via evaporation and condensation) and momentum (e.g., via wind stresses at the ocean surface).
See Also
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2014 Springer-Verlag Berlin Heidelberg
About this entry
Cite this entry
Grenfell, J.L. (2014). AOGCM. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5313-1
Download citation
DOI: https://doi.org/10.1007/978-3-642-27833-4_5313-1
Received:
Accepted:
Published:
Publisher Name: Springer, Berlin, Heidelberg
Online ISBN: 978-3-642-27833-4
eBook Packages: Springer Reference Physics and AstronomyReference Module Physical and Materials ScienceReference Module Chemistry, Materials and Physics