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    A METHOD OF REPRESENTING THE HORIZONTAL PRESSURE FORCE WITHOUT REDUCTION OF STATION PRESSURES TO SEA LEVEL 

    Source: Journal of Meteorology:;1960:;volume( 017 ):;issue: 002:;page 166
    Author(s): Sangster, Wayne E.
    Publisher: American Meteorological Society
    Abstract: A coordinate system is presented in which the lowest coordinate surface represents the topography of the earth. Higher coordinate surfaces reflect this topography in diminishing degrees and become isobaric at and above the ...
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    Source: Weather and Forecasting:;1990:;volume( 005 ):;issue: 004:;page 671
    Author(s): Sangster, Wayne E.
    Publisher: American Meteorological Society
    Abstract: No abstract available
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    An Improved Technique for Computing the Horizontal Pressure-Gradient Force at the Earth's Surface 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 007:;page 1358
    Author(s): Sangster, Wayne E.
    Publisher: American Meteorological Society
    Abstract: On conventional surface analyses, sea level isobars allow a forecaster to compute the horizontal pressure-gradient force at sea level, which for much of the world is fairly close to the earth's surface. However, over ...
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    Combining Precipitation Probabilities 

    Source: Monthly Weather Review:;1979:;volume( 107 ):;issue: 005:;page 520
    Author(s): Hughes, Lawrence A.; Sangster, Wayne E.
    Publisher: American Meteorological Society
    Abstract: Two methods are discussed for combining the routine forecasts of the 12 h probability of precipitation made by the National Weather Service, for use when longer period probabilities are desired but cannot be created ...
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    Precipitation Probability-Comparing Offices for Skill 

    Source: Monthly Weather Review:;1979:;volume( 107 ):;issue: 009:;page 1128
    Author(s): Hughes, Lawrence A.; Sangster, Wayne E.
    Publisher: American Meteorological Society
    Abstract: Using screening regression procedures, an attempt has been made to standardize probability of precipitation Brier scores for difficulty. Climatological factors affecting the difficulty of forecasting used are: precipitation ...
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