Stochastic dynamics of baroclinic waves

• Published in: Journal of the atmospheric sciences Vol. 50; no. 24; pp. 4044 - 4057
• Main Authors: Farrell, Brian F., Ionannou, Petros J.
• Format: Journal Article
• Language: English
• Published: Legacy CDMS American Meteorological Society 15.12.1993
• Subjects: Atmosphere; Climate; Earth, ocean, space; Exact sciences and technology; External geophysics; Heat; Meteorology; Meteorology And Climatology; Other topics in atmospheric geophysics; Baroclinic mode; Stochastic process; Shear flow; Heat transfer; Variance
• ISSN: 0022-4928; 1520-0469
• DOI: 10.1175/1520-0469(1993)050<4044:SDOBW>2.0.CO;2

The maintenance of variance and attendant heat flux in linear, forced dissipative baroclinic shear flows subject to stochastic excitation is examined. The baroclinic problem, is intrinsically nonnormal and its stochastic dynamics is found to differ significantly from the more familiar stochastic dynamics of normal systems. When the shear is sufficiently great in comparison to dissipative effects, stochastic excitation supports highly enhanced variance levels in these nonnormal systems compared to variance levels supproted by the same forcing and dissipation in related normal systems. The eddy variance and associated heat flux are found to arise in response to transient amplification of a subset of forcing functions that obtain energy from the mean flow and project this energy on a distinct subset of response functions (EOFs) that are in turn distinct from the set of normal modes of the system. A method for obtaining the dominant forcing and response functions as well as the distribution of heat flux for a given flow is described.