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    The Australian Summertime Cool Change. Part I: Synoptic and Subsynoptic Scale Aspects 

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 002:;page 177
    Author(s): Wilson, K. J.; Stern, H.
    Publisher: American Meteorological Society
    Abstract: In this, the first of a series of three papers on the structure of be summertime cool change of southeastern Australia, the prevailing climatological conditions are established, a background given to each of the cool changes ...
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    The Australian Summertime Cool Change. Part III: Subsynoptic and Mesoscale Model 

    Source: Monthly Weather Review:;1985:;volume( 113 ):;issue: 002:;page 224
    Author(s): Ryan, B. F.; Wilson, K. J.
    Publisher: American Meteorological Society
    Abstract: Observations of the Australian summertime cool change have ranged over both the subsynoptic scale (200?2000 km) and the mesoscale (20?200 km). In this paper, the final in a series of three, a conceptual subsynoptic and ...
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    An Approach to Verifying Prognoses of Line Phenomena and its Application to Fronts over Southeastern Australia 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 007:;page 1339
    Author(s): Wilson, K. J.; Barrell, S. L.; Beato, R. Del
    Publisher: American Meteorological Society
    Abstract: An approach to verifying position forecasts of line phenomena was developed. The technique, which tests for occurrence/nonoccurrence and the time of arrival of line phenomena, was applied to frontal position prognoses over ...
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    Modification of the Thermodynamic Structure of the Lower Troposphere by the Evaporation of Precipitation ahead of a Cold Front 

    Source: Monthly Weather Review:;1989:;volume( 117 ):;issue: 001:;page 138
    Author(s): Ryan, B. F.; Wilson, K. J.; Zipser, E. J.
    Publisher: American Meteorological Society
    Abstract: The evolution of an oceanic prefrontal subcloud layer of continental origin was examined by analyzing data gathered on the subsynoptic and mesoscale during Phase III of the Australian Cold Fronts Research Program. ...
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    Prefrontal Troughs over Southern Australia. Part I: A Climatology 

    Source: Weather and Forecasting:;1990:;volume( 005 ):;issue: 001:;page 22
    Author(s): Hanstrum, B. N.; Wilson, K. J.; Barrell, S. L.
    Publisher: American Meteorological Society
    Abstract: A climatology of the prefrontal westerly trough of southern Australia is presented, based on data for the 10-yr period 1976?85. Trough formation was confined to the longitudes of the Australian continent in the warmer ...
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    Prefrontal Troughs over Southern Australia. Part II: A Case Study of Frontogenesis 

    Source: Weather and Forecasting:;1990:;volume( 005 ):;issue: 001:;page 32
    Author(s): Hanstrum, B. N.; Wilson, K. J.; Barrell, S. L.
    Publisher: American Meteorological Society
    Abstract: A case study of frontogenesis within a surface prefrontal trough over southern Australia is presented. The trough developed ahead of a surface cold front and, over a period of approximately 24 h, intensified into a mature ...
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    Cold Fronts Research: The Australian Summertime “Cool Change” 

    Source: Bulletin of the American Meteorological Society:;1982:;volume( 063 ):;issue: 009:;page 1028
    Author(s): Smith, R. K.; Ryan, B. F.; Troup, A. J.; Wilson, K. J.
    Publisher: American Meteorological Society
    Abstract: Much of the significant weather of southeastern Australia is associated with the passage of cold fronts. In summer, such passages are often accompanied by rapid and extreme temperature fails, as hot continental northerly ...
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    Cold Fronts Research Programme: Progress, Future Plans, and Research Directions 

    Source: Bulletin of the American Meteorological Society:;1985:;volume( 066 ):;issue: 009:;page 1116
    Author(s): Ryan, B. F.; Garratt, J. R.; Wilson, K. J.; Smith, R. K.
    Publisher: American Meteorological Society
    Abstract: Following the analysis of data collected during Phases land II of the Cold Fronts Research Programme (CFRP) a conceptual model for the Australian summertime ?cool change? has been proposed. The model provides a focus and ...
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