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    The Propagation of Gravity–Inertia Waves and Lee Waves under a Critical Level 

    Source: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 011:;page 1505
    Author(s): Wurtele, M. G.; Datta, A.; Sharman, R. D.
    Publisher: American Meteorological Society
    Abstract: As is well known, the linear dynamic equations for gravity-inertia waves are characterized by three singular levels, one being the critical level at which flow speed and wave speed are equal, and the other two at which the ...
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    The Propagation of a Gravity–Inertia Wave in a Positively Sheared Flow 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 022:;page 3703
    Author(s): Wurtele, M. G.; Datta, A.; Sharman, R. D.
    Publisher: American Meteorological Society
    Abstract: When a gravity?inertia wave in two dimensions is generated by flow over a stationary boundary above the critical level, its vertical propagation will depend on whether it encounters the singular level at which kU/f is equal ...
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    Unsteadiness and Periodicity in Gravity Waves and Lee Waves Forced by a Fixed Rigid Boundary 

    Source: Journal of the Atmospheric Sciences:;1999:;Volume( 056 ):;issue: 014:;page 2269
    Author(s): Wurtele, M. G.; Datta, A.; Sharman, R. D.
    Publisher: American Meteorological Society
    Abstract: It is shown that a vertically sheared, inviscid stratified flow over a sinusoid, starting from rest, results in one of two responses, both nonsteady: 1) resonance modes, in which the phase lines are vertical, and wave ...
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