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    Suppression of Baroclinic Instability in Horizontally Sheared Flows 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 024:;page 3710
    Author(s): James, I. N.
    Publisher: American Meteorological Society
    Abstract: Baroclinic instability in the presence of a meridionally sheared barotropic component to the basic flow is studied using a two-level model. The inclusion of a linear shear results in merldionally confined normal modes with ...
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    Some Comparisons of Atmospheric Internal and Boundary Baroclinic Instability 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 020:;page 2142
    Author(s): James, I. N.; Hoskins, B. J.
    Publisher: American Meteorological Society
    Abstract: The existence of boundary baroclinic instability (as exemplified by the Eady or Charney problems) and internal baroclinic instability, which requires the potential vorticity gradient to take both signs in the fluid interior, ...
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    On the Differences between the Lifecycles of Some Baroclinic Waves Using the Primitive and Quasi-Geostrophic Equations on a Sphere 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 007:;page 741
    Author(s): MacVean, M. K.; James, I. N.
    Publisher: American Meteorological Society
    Abstract: Lifecycles of baroclinic waves obtained by integrating the primitive and quasi-geostrophic equations on the sphere are compared. Two basic states are considered. The first is based on Northern Hemisphere winter climatology, ...
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