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    Quasi-geostrophic Ocean Response to Real Wind Forcing: The Effects of Temporal Smoothing 

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 007:;page 998
    Author(s): Large, W. G.; Holland, W. R.; Evans, J. C.
    Publisher: American Meteorological Society
    Abstract: A one-degree, flat bottom, eight-layer quasi-geostrophic model of the North Pacific Ocean is forced by six different wind stress curl datasets, all derived from seven years of twice daily analyses at the European Centre ...
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    Separation of Warm-Core Rings in the Gulf of Mexico 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 002:;page 250
    Author(s): Sturges, W.; Evans, J. C.; Welsh, S.; Holland, W.
    Publisher: American Meteorological Society
    Abstract: The separation of anticyclonic rings is studied using a 12-level primitive equation numerical model of the western North Atlantic. The ?Gulf Stream Formation Region? model is based on the Bryan-Cox-Semtner code, and uses ...
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    Correlation Between Surface Gulf Stream and Bottom Flow New 5000 Meters Depth 

    Source: Journal of Physical Oceanography:;1982:;Volume( 012 ):;issue: 010:;page 1150
    Author(s): Kelley, E. A.; Weatherly, G. L.; Evans, J. C.
    Publisher: American Meteorological Society
    Abstract: Spectral analyses of three long-term (8 months), deep (?5 km), current-meter records located on the Scotian Rise (?40°N, 62°W) and a time series of the average northerly position of the surface Gulf Stream System obtained ...
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