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    Some Coolness Concerning Global Warming 

    Source: Bulletin of the American Meteorological Society:;1990:;volume( 071 ):;issue: 003:;page 288
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    On the Consistency of Thermistor Measurements of Upper Air Temperatures 

    Source: Journal of the Atmospheric Sciences:;1967:;Volume( 024 ):;issue: 003:;page 317
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Supersaturation of Vertically Propagating Internal Gravity Waves 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 004:;page 705
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: The usual assumption that vertically propagating internal gravity waves will cease growing with height once their amplitudes are such as to permit convective instability anywhere within the wave is reexamined. Two factors ...
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    On the Development of the Theory of the QBO 

    Source: Bulletin of the American Meteorological Society:;1987:;volume( 068 ):;issue: 004:;page 329
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: Recollections of the discovery of the quasi-biennial oscillation (QBO)of the equatorial stratosphere, and of the development of our present theoretical understanding of this phenomenon are presented.
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    The Eady Problem for a Basic State with Zero PV Gradient but β ≠ 0 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 022:;page 3221
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: The classic Eady problem is modified to include ? ? 0, but with the basic distributions of temperature and zonal flow adjusted to preserve zero meridional gradients of basic-state potential vorticity in the fluid interior. ...
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    The Effect of Concentrated PV Gradients on Stationary Waves 

    Source: Journal of the Atmospheric Sciences:;1994:;Volume( 051 ):;issue: 023:;page 3455
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: The author reexamines the Charney?Drazin problem with special attention to the concentration of potential vorticity gradient in the neighborhood of the tropopause. It is found that the degree of concentration has a profound ...
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    The Radiative-Photochemical Response of the Mesosphere to Fluctuations in Radiation 

    Source: Journal of the Atmospheric Sciences:;1965:;Volume( 022 ):;issue: 005:;page 469
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: The response of the mesosphere to slow fluctuations in ultraviolet and visible radiation intensity is investigated using the simplified models for photochemistry and radiative transfer developed by Lindzen and Goody (1965). ...
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    ON THE THEORY OF THE DIURNAL TIDE 

    Source: Monthly Weather Review:;1966:;volume( 094 ):;issue: 005:;page 295
    Author(s): LINDZEN, RICHARD S.
    Publisher: American Meteorological Society
    Abstract: Laplace's tidal equation for diurnal tides of longitudinal number one is investigated. It is found that in addition to the previously found solutions (Hough Functions) corresponding to positive equivalent, depths there are ...
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    On the Relation of Wave Behavior to Source Strength and Distribution in a Propagating Medium 

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 005:;page 630
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Radiative and Photochemical Processes in Mesospheric Dynamics: Part IV, Stability of a Zonal Vortex at Mid-Latitudes to Baroclinic Waves 

    Source: Journal of the Atmospheric Sciences:;1966:;Volume( 023 ):;issue: 003:;page 350
    Author(s): Lindzen, Richard S.
    Publisher: American Meteorological Society
    Abstract: The models developed in Part I for radiative transfer and ozone photochemistry in the mesosphere are incorporated into a two-level model for baroclinic flow, and the effect of radiative and photochemical processes on the ...
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