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    Cyclonically Forced Barrier Winds along the Transantarctic Mountains near Ross Island 

    Source: Monthly Weather Review:;1994:;volume( 122 ):;issue: 001:;page 137
    Author(s): O'Connor, William P.; Bromwich, David H.; Carrasco, Jorge F.
    Publisher: American Meteorological Society
    Abstract: The effect of the Transantarctic Mountains on cyclonically forced boundary-layer winds in the vicinity of Ross Island, Antarctica (77.5°S, 167°E), is discussed. When cyclones are present over the western Ross Ice Shelf and ...
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    On the Net Cyclonic Circulation in Large Stratified Lakes 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 006:;page 1516
    Author(s): Schwab, David J.; O'Connor, William P.; Mellor, George L.
    Publisher: American Meteorological Society
    Abstract: This paper proposes a possible explanation for the mean cyclonic circulation in large stratified lakes The condition of no heat flux through the bottom boundary causes the isotherms to dip near the shores to intersect the ...
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    Forecast Verification for Eta Model Winds Using Lake Erie Storm Surge Water Levels 

    Source: Weather and Forecasting:;1999:;volume( 014 ):;issue: 001:;page 119
    Author(s): O’Connor, William P.; Schwab, David J.; Lang, Gregory A.
    Publisher: American Meteorological Society
    Abstract: This article has two purposes. The first is to describe how the Great Lakes Coastal Forecasting System (GLCFS) can be used to validate wind forecasts for the Great Lakes using observed and forecast water levels. The second ...
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    Numerical Simulation of Internal Kelvin Waves and Coastal Upwelling Fronts 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 007:;page 1197
    Author(s): Beletsky, Dmitry; O’Connor, William P.; Schwab, David J.; Dietrich, David E.
    Publisher: American Meteorological Society
    Abstract: Two three-dimensional primitive equation numerical ocean models are applied to the problem of internal Kelvin waves and coastal upwelling in the Great Lakes. One is the Princeton Ocean Model (POM) with a terrain-following ...
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