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On the behaviour of baroclinic waves undergoing horizontal deformation. I: The ‘ RT ’ phase diagram
Author(s) -
Bishop Craig H.
Publication year - 1993
Publication title -
quarterly journal of the royal meteorological society
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.744
H-Index - 143
eISSN - 1477-870X
pISSN - 0035-9009
DOI - 10.1002/qj.49711951002
Subject(s) - baroclinity , cyclogenesis , vorticity , diagram , mechanics , modal , geology , potential vorticity , shear (geology) , deformation (meteorology) , classical mechanics , physics , mathematics , vortex , meteorology , materials science , computer science , cyclone (programming language) , statistics , field programmable gate array , polymer chemistry , computer hardware , petrology
Non‐modal baroclinic wave growth in an idealizsed flow comprising baroclinic shear and horizontal confluence is considered. It is shown how a general semi‐analytic solution may be derived for the evolution of non‐modal waves with uniform potential vorticity in this ‘mixed’ basic state. The solution is new. It represents a synthesis of baroclinic waves with pure deformation solutions. For a given initial wavelength the solution is capable of describing an infinite number of distinct non‐modal developments. To overview this large variety, phase diagrams, dubbed ‘ RT ’ diagrams, have been developed. The diagrams depict the evolution of vertical structure for a wide range of initial conditions. Some specific solutions with relevance to type B cyclogenesis and the potentially destablizing effect of deformation are discussed.

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