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    Role of the Low-Frequency Deformation Field on the Explosive Growth of Extratropical Cyclones at the Jet Exit. Part II: Baroclinic Critical Region 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 008:;page 1982
    Author(s): Rivière, G.; Joly, A.
    Publisher: American Meteorological Society
    Abstract: Midlatitude cyclones tend to develop strongly in specific locations relative to the large-scale flow, such as jet-exit zones. Here, the approach developed in Part I that highlights the role of large-scale deformation in ...
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    Role of the Low-Frequency Deformation Field on the Explosive Growth of Extratropical Cyclones at the Jet Exit. Part I: Barotropic Critical Region 

    Source: Journal of the Atmospheric Sciences:;2006:;Volume( 063 ):;issue: 008:;page 1965
    Author(s): Rivière, G.; Joly, A.
    Publisher: American Meteorological Society
    Abstract: By using new theoretical results on perturbation growth in spatially and temporally complex quasigeostrophic flows, this paper investigates the role of the large-scale deformation field on extratropical cyclones and ...
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    Consequences of the Geostrophic Momentum Approximation on Barotropic Instability 

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 001:;page 103
    Author(s): Malardel, S.; Thorpe, A. J.; Joly, A.
    Publisher: American Meteorological Society
    Abstract: A subsynoptic instability with dominant barotropic signature has been found to be a possible mechanism for the development of frontal waves. Linear semigeostrophic calculations of the growth rate of waves developing along ...
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    Is a Real Cyclogenesis Case Explained by Generalized Linear Baroclinic Instability? 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 012:;page 4287
    Author(s): Descamps, L.; Ricard, D.; Joly, A.; Arbogast, P.
    Publisher: American Meteorological Society
    Abstract: Midlatitude cyclogenesis is currently often explained as resulting from the baroclinic instability of a jet flow. The present formulation of the theory, essentially resulting from the deep revision performed by Farrell, ...
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