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    THE ONSET OF RAIN FROM CUMULI 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 005:;page 354
    Author(s): Langwell, Patricia A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    A MECHANISM FOR CONVECTION OVER THE OCEAN 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 003:;page 187
    Author(s): Langwell, Patricia A.
    Publisher: American Meteorological Society
    Abstract: The cumuli which form over the ocean near Puerto Rico cannot be the result of ?thermals.? A theory is evolved, based on the oscillation of the boundary between the well-mixed layer near the ocean and the cloud layer. The ...
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    INHOMOGENETIES OF TURBULENCE, TEMPERATURE, AND MOISTURE IN THE WEST INDIES TRADE-WIND REGIONS 

    Source: Journal of Meteorology:;1948:;volume( 005 ):;issue: 005:;page 243
    Author(s): Langwell, Patricia A.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    STATISTICAL PROPERTIES OF PRESSURE CHANGE ALOFT 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 003:;page 172
    Author(s): Kaciak, William; Langwell, Patricia A.
    Publisher: American Meteorological Society
    Abstract: The basis of many statistical tests is the assumption that the data are drawn from a normal population. The change in pressure over one to ten days at 3000 dynamic meters, at 50°N and 70°W, is tested, and the circumstances ...
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