Abstract
The low-order, nine-component, primitive equation model of Lorenz (1980) is used as the basis for a comparative study of the quality of several intermediate models. All the models are intermediate between the primitive equations and quasi-geostrophy and will not support gravity-wave oscillations; this reduces to three the number of independent components in each. Strange attractors, stable limit cycles, and stable and unstable fixed points are found in the models.-from Author
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CITATION STYLE
Gent, P. R., & McWilliams, J. C. (1982). Intermediate model solutions to the Lorenz equations: strange attractors and other phenomena. Journal of the Atmospheric Sciences, 39(1), 3–13. https://doi.org/10.1175/1520-0469(1982)039<0003:IMSTTL>2.0.CO;2
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