American Geophysical Union Become an AGU Member
Subscribe to AGU Journals
AGU Home AGU Publications

Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF, file size: 1077306 bytes)

GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L22801, doi:10.1029/2007GL031779, 2007

Recovery of atmospheric flow statistics in a general circulation model without nonlinear eddy-eddy interactions

Paul A. O'Gorman

California Institute of Technology, Pasadena, California, USA


Tapio Schneider

California Institute of Technology, Pasadena, California, USA


Abstract

The closure problem of turbulence arises because nonlinear interactions among turbulent fluctuations (eddies) lead to an infinite hierarchy of moment equations for flow statistics. Here we demonstrate with an idealized general circulation model (GCM) that many atmospheric flow statistics can already be recovered if the hierarchy of moment equations is truncated at second order, corresponding to the elimination of nonlinear eddy-eddy interactions. Some, but not all, features of the general circulation remain the same. The atmospheric eddy kinetic energy spectrum retains a −3 power-law range even though this is usually explained in terms of an enstrophy cascade mediated by nonlinear eddy-eddy interactions. Our results suggest that it may be possible to construct fast general circulation models that solve for atmospheric flow statistics directly rather than via simulation of individual eddies and their interactions.

Received 22 August 2007; accepted 12 October 2007; published 16 November 2007.

Keywords: turbulence; general circulation model; energy spectrum.

Index Terms: 3379 Atmospheric Processes: Turbulence (4490); 3319 Atmospheric Processes: General circulation (1223); 3367 Atmospheric Processes: Theoretical modeling.


Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF, file size: 1077306 bytes)

Citation: O'Gorman, P. A., and T. Schneider (2007), Recovery of atmospheric flow statistics in a general circulation model without nonlinear eddy-eddy interactions, Geophys. Res. Lett., 34, L22801, doi:10.1029/2007GL031779.