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    A Two-Layer Quasi-Geostrophic Model of Summer Trough Formation in the Australian Subtropical Easterlies 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 005:;page 807
    Author(s): Fandry, C. B.; Leslie, L. M.
    Publisher: American Meteorological Society
    Abstract: A dominant feature of the low-level easterly wind flow in the Australian subtropics during summer is the trough development that occurs on both the western and eastern sides of the continent. This phenomenon is investigated ...
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    A Simple Topographic Model of Gulf Stream Separation 

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 001:;page 22
    Author(s): Smith, Neville R.; Fandry, C. B.
    Publisher: American Meteorological Society
    Abstract: A simple, frictional, linear model is used to study the motion of the Gull Stream over the continental shelf. It is found that the combination of frictional and topographic effects may provide a further mechanism by which ...
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    Kelvin-Type Coastal Surges Generated by Tropical Cyclones 

    Source: Journal of Physical Oceanography:;1984:;Volume( 014 ):;issue: 003:;page 582
    Author(s): Fandry, C. B.; Leslie, L. M.; Steedman, R. K.
    Publisher: American Meteorological Society
    Abstract: Measurements of sea level along the coat of Western Australia during the period 1969 to 1982. when 12 southward moving tropical cyclones occurred, showed distinct peaks with amplitudes of about 1 to 2 m propagating southwards ...
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