Mathematics – Logic
Scientific paper
Jul 1988
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988qjrms.114.1063o&link_type=abstract
Royal Meteorological Society, Quarterly Journal (ISSN 0035-9009), vol. 114, July 1988, p. 1063-1110.
Mathematics
Logic
57
Atmospheric Boundary Layer, Atmospheric Models, Computerized Simulation, Perturbation Theory, Stratosphere, Meridional Flow, Mesosphere, Numerical Flow Visualization, Planetary Waves, Troposphere, Zonal Flow (Meteorology)
Scientific paper
The dynamics of linear and nonlinear, large-scale disturbances generated in the stratosphere by a localized perturbation in the troposphere are studied and compared. The perturbation is applied at the lower boundary of a primitive equation model of the stratosphere and mesosphere. The simulations are contrasted with an idealized theoretical model of a nonlinear critical layer. It is suggested that regarding the troposphere as a wavemaker forcing changes in the stratosphere according to the tenets of wave, mean-flow theory is an oversimplification. It is found that, preceding a major warming, the flow is asymmetric about any axis and strong warmings develop through the nonlinear interaction of large, deep vortices associated with a tropospheric asymmetry. Associated changes in zonal mean winds give the appearance of distinct minor and major warmings, though a synoptic view allows systematic changes to be seen which caution against dividing the evolution into separate events.
O'Neill Alan
Pope V. D.
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