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    The Mixing of Mass and Momentum by Kelvin-Helmboltz Billows 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 014:;page 2509
    Author(s): Scinocca, J. F.
    Publisher: American Meteorological Society
    Abstract: The mixing of mass and momentum induced by the full life cycle of stratified shear instability is considered. In particular, the nonlinear numerical simulation of a stratified shear layer that is unstable to Kelvin?Helmholtz ...
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    The Nonlinear Forcing of Large-Scale Internal Gravity Waves by Stratified Shear Instability 

    Source: Journal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 005:;page 653
    Author(s): Scinocca, J. F.; Ford, R.
    Publisher: American Meteorological Society
    Abstract: The forcing of large-scale internal gravity waves by shear-unstable stratified free shear layers is investigated. The gravity wave forcing mechanism considered arises from the nonlinear interaction of unstable modes of ...
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    The Origin of Severe Downslope Windstorm Pulsations 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 024:;page 2853
    Author(s): Peltier, W. R.; Scinocca, J. F.
    Publisher: American Meteorological Society
    Abstract: Recently reported Doppler lidar observations of the downslope component of flow velocity made during the occurrence of a mountain windstorm at Boulder, Colorado, have established that such storms are characterized by an ...
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    On The Richardson Number Dependence of Nonlinear Critical-Layer Flow over Localized Topography 

    Source: Journal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 013:;page 1560
    Author(s): Scinocca, J. F.; Peltier, W. R.
    Publisher: American Meteorological Society
    Abstract: The dynamics of stratified shear flow over localized topography in two spatial dimensions is investigated through analysis of a sequence of nonlinear numerical simulations. The existence of a critical level for all stationary ...
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    Pulsating Downslope Windstorms 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 018:;page 2885
    Author(s): Scinocca, J. F.; Peltier, W. R.
    Publisher: American Meteorological Society
    Abstract: The flow configurations that obtain in several severe downslope windstorm events generated over isolated topography are studied using a two-dimensional nonlinear anelastic model. A new high resolution simulation of the 11 ...
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    The Instability of Long's Stationary Solution and the Evolution toward Severe Downslope Windstorm Flow. Part I: Nested Grid Numerical Simulations 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 014:;page 2245
    Author(s): Scinocca, J. F.; Peltier, W. R.
    Publisher: American Meteorological Society
    Abstract: Through direct numerical simulation, the instability of Long's exact finite-amplitude steady-state solution to the problem of stratified flow over topography and the subsequent evolution towards severe downslope windstorm ...
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    The Instability of Long's Stationary Solution and the Evolution toward Severe Downslope Windstorm Flow. Part II: The Application of Finite-Amplitude Local Wave-Activity Flow Diagnostics 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 004:;page 623
    Author(s): Scinocca, J. F.; Peltier, W. R.
    Publisher: American Meteorological Society
    Abstract: An analysis of severe downslope windstorm evolution, from flow conditions initially described by Long's stationary solution, is considered through the application of finite-amplitude wave-activity diagnostics. Such quantities ...
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    Finite-Amplitude Wave-Activity Diagnostics for Long's Stationary Solution 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 004:;page 613
    Author(s): Scinocca, J. F.; Peltier, W. R.
    Publisher: American Meteorological Society
    Abstract: Finite-amplitude wave-activity diagnostics characteristic of the steady-state flow of a stratified Boussinesq fluid over localized topography in two spatial dimensions are considered. In particular, analytic expressions ...
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    Nonlinear Wave-Activity Conservation Laws and Hamiltonian Structure for the Two-Dimensional Anelastic Equations 

    Source: Journal of the Atmospheric Sciences:;1992:;Volume( 049 ):;issue: 001:;page 5
    Author(s): Scinocca, J. F.; Shepherd, T. G.
    Publisher: American Meteorological Society
    Abstract: Exact, finite-amplitude, local wave-activity conservation laws are derived for disturbances to steady flows in the context of the two-dimensional anelastic equations. The conservation laws are expressed entirely in terms ...
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    Coordinated Global and Regional Climate Modeling 

    Source: Journal of Climate:;2015:;volume( 029 ):;issue: 001:;page 17
    Author(s): Scinocca, J. F.; Kharin, V. V.; Jiao, Y.; Qian, M. W.; Lazare, M.; Solheim, L.; Flato, G. M.; Biner, S.; Desgagne, M.; Dugas, B.
    Publisher: American Meteorological Society
    Abstract: new approach of coordinated global and regional climate modeling is presented. It is applied to the Canadian Centre for Climate Modelling and Analysis Regional Climate Model (CanRCM4) and its parent global climate model ...
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