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    Saturated and Unsaturated Spectra of Gravity Waves and Scale-Dependent Diffusion 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 018:;page 2211
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: For a highly idealized condition, the spectrum of saturated and unsaturated gravity waves at each height is calculated directly from the wave equation. A principal feature of this wave equation is the inclusion of wave ...
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    Energy Dissipation Rates of Turbulence in the Stable Free Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 004:;page 880
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: For stable stratification, it is pointed out that there exists a strong correlation between the intensity of atmospheric turbulence and the energy dissipation rate ?. It is given in terms of the variance of vertical velocity ...
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    A Theory of Gaps in the Turbulence Spectra of Stably Stratified Shear Flows 

    Source: Journal of the Atmospheric Sciences:;1980:;Volume( 037 ):;issue: 007:;page 1542
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: A gap and adjacent bump is predicted to occur in the velocity spectrum of stratified shear flows when the flux Richardson number Rf, ?1/2. This prediction is based on a straightforward solution of the spectral energy balance ...
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    Finite Amplitude Gravity Waves: Harmonics, Advective Steepening and Saturation 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 007:;page 688
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: Steepening, harmonics generation, and saturation of a finite amplitude gravity wave are calculated in an approximate fashion by means of a new and elementary approach. The mechanism for these phenomena is nonlinear advection. ...
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    Nonlinear Theory of Gravity Waves: Momentum Deposition, Generalized Rayleigh Friction, and Diffusion 

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 008:;page 1698
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: A nonlinear theory of internal gravity waves is extended to slowly varying mean winds u0. This theory determines the wave amplitudes, enhanced diffusion and momentum deposition, for a broad spectrum of waves as well as for ...
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    On the Theory of Temperature Spectra in a Stably Stratified Fluid 

    Source: Journal of Physical Oceanography:;1985:;Volume( 015 ):;issue: 004:;page 475
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: It is shown that the Lumley-Phillips buoyancy subrange theory predicts the temperature spectrum to be proportional to k?3 at small scalar wavenumbers k?-consistent with oceanic experiments (although those experiments measure ...
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    Vertical Turbulent Diffusion in a Stably Stratified Fluid 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 006:;page 1022
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: The vertical turbulent diffusion coefficient in a stably stratified fluid is derived analytically. This derivation does not require that the flux Richardson number be known or specified. The resulting expression for the ...
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    On the Theory of Turbulence in the Buoyancy Subrange of Stably Stratified Flows 

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 004:;page 634
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: A theoretical investigation is made of turbulence in the buoyancy subrange of stably stratified sheer flows. This theory is based on a new calculation of the buoyancy flux spectrum B (k). In the Lumley-Shur theory, it was ...
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    Superadiabatic Excess and Gravity Wave Saturation 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 022:;page 3519
    Author(s): Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: Attention is called to a recent calculation of the superadiabatic excess?the ratio of wave amplitude at saturation to wave amplitude at convective instability threshold?caused by a saturated gravity wave. (This excess is ...
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    The Stokes Drift due to Vertically Propagating Internal Gravity Waves in a Compressible Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 022:;page 2636
    Author(s): Coy, Lawrence; Fritts, David C.; Weinstock, J.
    Publisher: American Meteorological Society
    Abstract: Vertically propagating, compressible, internal gravity waves are shown to have a vertical Stokes drift which is proportional to the vertical wave energy flux. In regions of the atmosphere dominated by upward propagating ...
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