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    A Diagnostic Case Study of the Synoptic Scale Vertical Motion and its Contribution to Mid-Tropospheric Development 

    Source: Journal of Applied Meteorology:;1964:;volume( 003 ):;issue: 006:;page 669
    Author(s): Stuart, David W.
    Publisher: American Meteorological Society
    Abstract: The quasi-geostrophic omega equation is employed to perform a diagnostic case study of the baroclinic structure of a developing system. The model employs height data at ten pressure levels to obtain the vertical motion ...
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    A Comparison of Quasi-Geostrophic Vertical Motion Using Various Analyses 

    Source: Monthly Weather Review:;1974:;volume( 102 ):;issue: 005:;page 363
    Author(s): Stuart, David W.
    Publisher: American Meteorological Society
    Abstract: Three subjective and two objective analysis techniques were employed to prepare height data for a synoptic case over North America. These heights were used as input to a ten-level quasi-geostrophic model for computation ...
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    Reply 

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 005:;page 324
    Author(s): STUART, DAVID W.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    Reply 

    Source: Monthly Weather Review:;1968:;volume( 096 ):;issue: 002:;page 104
    Author(s): STUART, DAVID W.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available.
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    The Structure of the Marine Inversion in Northwest Oregon during 26–30 August 1973 

    Source: Monthly Weather Review:;1977:;volume( 105 ):;issue: 006:;page 748
    Author(s): Meitín, Rebecca Jo; Stuart, David W.
    Publisher: American Meteorological Society
    Abstract: As a part of the Second Coastal Upwelling Experiment along the Oregon Coast in summer 1973, extensive thermodynamic data were gathered in a mesoscale area. These data were examined in relation to the marine inversion at ...
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    Low-Level Atmospheric Changes over Oregon's Coastal Upweliing Region 

    Source: Monthly Weather Review:;1980:;volume( 108 ):;issue: 007:;page 1029
    Author(s): Hawkins, Jefrey D.; Stuart, David W.
    Publisher: American Meteorological Society
    Abstract: Temporal and spatial variations in the structure of the lower atmosphere off Oregon's central coast are studied. The response of the wind and thermal fields to a synoptic-scale realignment aloft that causes a rapid shift ...
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    THE OVER-RELAXATION FACTOR IN THE NUMERICAL SOLUTION OF THE OMEGA EQUATION 

    Source: Monthly Weather Review:;1967:;volume( 095 ):;issue: 005:;page 303
    Author(s): STUART, DAVID W.; O'NEILL, THOMAS H. R.
    Publisher: American Meteorological Society
    Abstract: Results of tests for the optimum over-relaxation coefficients in the numerical relaxation of the omega equation are presented. One case considers a strong upper-level development for tests on a fixed grid using one-, two-, ...
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    Observations of the Coastal Upwelling Region near 34°30′N of California: Spring 1981 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 002:;page 378
    Author(s): Brink, Kenneth H.; Stuart, David W.; Van Leer, John C.
    Publisher: American Meteorological Society
    Abstract: Coordinated meteorological and oceanographic (CTD) measurements were made near Point Conception, California, during March?April 1981. The goal of the observations was to study coastal upwelling and the local characteristics ...
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