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    Implications of Monin–Obukhov Similarity Theory for Scalar Quantities 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 014:;page 2236
    Author(s): Hill, Reginald J.
    Publisher: American Meteorological Society
    Abstract: Monin-Obukhov similarity theory of surface-layer turbulence has been extended to include all scalar quantities. The tenets of this theory, as it is presently practiced, are followed to their logical conclusions, which ...
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    Structure Functions and Spectra of Scalar Quantities in the Inertial–Convective and Viscous–Convective Ranges of Turbulence 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 046 ):;issue: 014:;page 2245
    Author(s): Hill, Reginald J.
    Publisher: American Meteorological Society
    Abstract: The Obukhov?Corrsin constants (often referred to as Kolmogorov constants) are the constants of proportionality in formulas pertaining to the inertial-convective range of structure functions (or spectra) of scalar quantities ...
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    A Note on the 26-Month Oscillation 

    Source: Journal of the Atmospheric Sciences:;1964:;Volume( 021 ):;issue: 003:;page 320
    Author(s): Newell, Reginald E.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Note on Nocturnal Radiation Reversal 

    Source: Monthly Weather Review:;1972:;volume( 100 ):;issue: 005:;page 354
    Author(s): CLARKE, REGINALD H.
    Publisher: American Meteorological Society
    Abstract: Nocturnal radiation reversal is essentially an unsteady, advective effect. It requires that clouds or fog drift over a previously cooled surface. In the case of higher clouds, reversal can occur only with a sufficiently ...
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    Numerical Modeling of a Case of Nocturnal Radiation Reversal 

    Source: Monthly Weather Review:;1972:;volume( 100 ):;issue: 005:;page 357
    Author(s): CLARKE, REGINALD H.
    Publisher: American Meteorological Society
    Abstract: A one-dimensional boundary-layer model is used to simulate a rare occurrence of nocturnal radiation reversal, with measured downward radiation and horizontal pressure and temperature gradients regarded as given. The time ...
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    El Niño: An Approach Towards Equilibrium Temperature in the Tropical Eastern Pacific 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 007:;page 1338
    Author(s): Newell, Reginald E.
    Publisher: American Meteorological Society
    Abstract: A different view of El Niño is proposed, namely, that it represents an approach towards the tropical equilibrium temperature of approximately 30°C, set essentially by evaporation, by the waters of the eastern tropical Pacific.
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    Stratospheric Temperature Change from the Mt. Agung Volcanic Eruption of 1963 

    Source: Journal of the Atmospheric Sciences:;1970:;Volume( 027 ):;issue: 006:;page 977
    Author(s): Newell, Reginald E.
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Preliminary Study of Quasi-Horizontal Eddy Fluxes from Meteorological Rocket Network Data 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 003:;page 213
    Author(s): Newell, Reginald E.
    Publisher: American Meteorological Society
    Abstract: The meridional transport of relative angular momentum by transient eddies is computed from the wind data so far available from the Meteorological Rocket Network for the 25?60 km region. The transport is northward in winter ...
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    DRIFT ICE AND THE THEORY OF OCEAN CURRENTS 

    Source: Monthly Weather Review:;1900:;Volume( 028 ):;issue: 010:;page 433
    Author(s): Daly, Reginald A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Algorithms for Obtaining Atmospheric Surface-Layer Fluxes from Scintillation Measurements 

    Source: Journal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 003:;page 456
    Author(s): Hill, Reginald J.
    Publisher: American Meteorological Society
    Abstract: Algorithms are derived for obtaining atmospheric surface-layer fluxes of heat, humidity, and momentum from scintillation measurements. Both the three-wavelength and two-wavelength methods are examined, as is combining the ...
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