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    Intrusive Mixing in a Mediterranean Salt Lens—Intrusion Slopes and Dynamical Mechanisms 

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 011:;page 1274
    Author(s): Ruddick, Barry
    Publisher: American Meteorological Society
    Abstract: Thermohaline intrusions found in Meddy ?Sharon? were laterally coherent The slope of these intrusions across density surfaces was in opposite senses in the upper and lower part of the meddy, consistent with (i) the McIntyre ...
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    A Generalized Solution for the Large-Scale, Time-Average Perturbations in the Atmosphere 

    Source: Journal of the Atmospheric Sciences:;1963:;Volume( 020 ):;issue: 003:;page 226
    Author(s): Saltzman, Barry
    Publisher: American Meteorological Society
    Abstract: A solution is given, in the form of influence functions, for the forced geostrophic response of the atmosphere to the combined effects of zonal asymmetries in (i) the lower boundary orography and (ii) the mean, ...
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    Dynamic Behavior and Design of Fatigue Test Specimens 

    Source: Journal of Manufacturing Science and Engineering:;1971:;volume( 093 ):;issue: 001:;page 340
    Author(s): Barry Wolf
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: In tension-tension, as well as in compression-tension, fatigue testing it has been observed that there exist combinations of loading and specimen characteristics for which the specimen becomes ...
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    ON THE THEORY OF THE WINTER-AVERAGE PERTURBATIONS IN THE TROPOSPHERE AND STRATOSPHERE 

    Source: Monthly Weather Review:;1965:;volume( 093 ):;issue: 004:;page 195
    Author(s): SALTZMAN, BARRY
    Publisher: American Meteorological Society
    Abstract: A general solution is obtained for forced, stationary, quasi-geostrophic perturbations in an atmosphere having the main zonal-average characteristics of the winter troposphere and stratosphere. Special solutions along 45° ...
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    On the Role of Equilibrium Atmospheric Climate Models in the Theory of Long-Period Glacial Variations 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 014:;page 2263
    Author(s): Saltzman, Barry
    Publisher: American Meteorological Society
    Abstract: No abstract available.
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    Climatic “Equilibrium” for the Quaternary 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 001:;page 109
    Author(s): Saltzman, Barry
    Publisher: American Meteorological Society
    Abstract: Not available
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    SOME HEMISPHERIC SPECTRAL STATISTICS 

    Source: Journal of Meteorology:;1958:;volume( 015 ):;issue: 003:;page 259
    Author(s): Saltzman, Barry
    Publisher: American Meteorological Society
    Abstract: The results of computations of the spectrum of the eddy kinetic energy, the angular momentum transport, and the transfer of kinetic energy between the eddies and the mean motion, for the month of January 1949, are presented. ...
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    Finite Amplitude Free Convection as an Initial Value Problem—I 

    Source: Journal of the Atmospheric Sciences:;1962:;Volume( 019 ):;issue: 004:;page 329
    Author(s): Saltzman, Barry
    Publisher: American Meteorological Society
    Abstract: The Oberbeck-Boussinesq equations are reduced to a two-dimensional form governing ?roll? convection between two free surfaces maintained at a constant temperature difference. These equations are then transformed to a set ...
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    The Quantitative Use of PIREPs in Developing Aviation Weather Guidance Products 

    Source: Weather and Forecasting:;1996:;volume( 011 ):;issue: 003:;page 372
    Author(s): Schwartz, Barry
    Publisher: American Meteorological Society
    Abstract: An evaluation of the utility of pilot reports (PIREPs) of weather for aviation forecasting product development is presented. Although PIREPs were never intended for quantitative use, this limitation has not prevented ...
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    EQUATIONS GOVERNING THE ENERGETICS OF THE LARGER SCALES OF ATMOSPHERIC TURBULENCE IN THE DOMAIN OF WAVE NUMBER 

    Source: Journal of Meteorology:;1957:;volume( 014 ):;issue: 006:;page 513
    Author(s): Saltsman, Barry
    Publisher: American Meteorological Society
    Abstract: By considering the Fourier analysis of the planetary field of motion in the atmosphere, it is possible to define ?scales? of motion and to write equations which govern the behavior of these separate scales of motion. ...
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