Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8953
AuthorsMasina, S.* 
Philander, S. G. H.* 
Bush, A. B. G.* 
TitleAn analysis of tropical instability waves in a numerical model of the Pacific Ocean - 2. Generation and energetics of the waves
Issue Date15-Dec-1999
Series/Report no.C12/104 (1999)
DOI10.1029/1999JC900226
URIhttp://hdl.handle.net/2122/8953
KeywordsOcean modeling
Equatorial Ocean
Tropical Instability Waves
Ocean wave generation
Ocean wave energetics
Subject Classification03. Hydrosphere::03.01. General::03.01.01. Analytical and numerical modeling 
AbstractThe instability processes which generate unstable waves with chara- cteristics similar to observed tropical instability waves in the Pacific Ocean are examined through a local energy analysis based on deviations from the time mean flow. Numerical experiments indicate that the waves develop preferentially in the eastern Pacific along the northern temperature front and have a westward phase speed and a structure with two peaks in amplitude: one located on the equator and the other a few degrees north of it. The energy analysis shows that the "two-peak" structure of the eastern waves is explained by two different instability processes which occur at different latitudes. In the time mean sense the region north of the equator is baroclinically unstable, while barotropic instability prevails at the equator. The life cycle of the waves is revealed by the time evolution of the energetics. Baroclinic instability is the dominant triggering mechanism which induces growth of the waves along the northern temperature front. The eddy pressure fluxes radiate energy south of the equator where the rneridional shear between the Equatorial Undercurrent and the South Equatorial Current becomes barotropically unstable. From the numerical simulations, there is evidence of a second unstable region in the central Pacific south of the equator where the instabilities have a lower phase speed. The energy analysis also shows that these waves grow from both barotropic and baroclinic conversions.
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