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    Relating Overreflection and Wave Geometry to the Counterpropagating Rossby Wave Perspective: Toward a Deeper Mechanistic Understanding of Shear Instability 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 007:;page 2238
    Author(s): Harnik, N.; Heifetz, E.
    Publisher: American Meteorological Society
    Abstract: The two major approaches to understanding plane parallel shear instability?the counterpropagating Rossby wave (CRW) and overreflection (OR) approaches?illuminate very different fundamental aspects. This work examines how ...
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    Apparent Absolute Instability and the Continuous Spectrum 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 021:;page 3592
    Author(s): Bishop, C. H.; Heifetz, E.
    Publisher: American Meteorological Society
    Abstract: The role of the continuous spectrum and its associated potential vorticity (PV) in absolute instability are investigated in the context of a semi-infinite version of Eady?s basic state. This flow crudely resembles the ...
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    A physical interpretation of the wind-wave instability as interacting waves 

    Source: Journal of Physical Oceanography:;2017:;Volume( 047 ):;issue: 006:;page 1441
    Author(s): Carpenter, J. R.; Guha, A.; Heifetz, E.
    Publisher: American Meteorological Society
    Abstract: ne mechanism for the growth of ocean surface waves by wind is through a shear instability that was first described by Miles (1957). We provide a physical interpretation of this wind-wave instability in terms of the interaction ...
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    On the Parcel Method and the Baroclinic Wedge of Instability 

    Source: Journal of the Atmospheric Sciences:;1998:;Volume( 055 ):;issue: 005:;page 788
    Author(s): Heifetz, E.; Alpert, P.; da Silva, A.
    Publisher: American Meteorological Society
    Abstract: The heuristic explanation, suggested by the parcel method, for the baroclinic instability mechanism is reexamined. The parcel method argues that an air parcel displaced within the wedge of instability, that is, between the ...
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    A Buoyancy–Vorticity Wave Interaction Approach to Stratified Shear Flow 

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 008:;page 2615
    Author(s): Harnik, N.; Heifetz, E.; Umurhan, O. M.; Lott, F.
    Publisher: American Meteorological Society
    Abstract: Motivated by the success of potential vorticity (PV) thinking for Rossby waves and related shear flow phenomena, this work develops a buoyancy?vorticity formulation of gravity waves in stratified shear flow, for which the ...
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