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    How Does the Deep Western Boundary Current Cross the Gulf Stream? 

    Source: Journal of Physical Oceanography:;1993:;Volume( 023 ):;issue: 012:;page 2602
    Author(s): Pickart, Robert S.; Smethie, William M.
    Publisher: American Meteorological Society
    Abstract: The manner in which the deep western boundary current (DWBC) crosses the Gulf Stream is investigated using data from a hydrographic survey conducted in 1990. Absolute geostrophic velocity vectors are computed using in situ ...
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    Determining the Strength of the Deep Western Boundary Current Using the Chlorofluoromethane Ratio 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 007:;page 940
    Author(s): Pickart, Robert S.; Hogg, Nelson G.; Smethie, William M.
    Publisher: American Meteorological Society
    Abstract: The dilution of a passive tracer during deep water formation and the subsequent advection/mixing in a deep boundary current is modeled with application to chlorofluoromethanes (CFMs) in the North Atlantic. Two different ...
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    Changes in the CFC Inventories and Formation Rates of Upper Labrador Sea Water, 1997–2001 

    Source: Journal of Physical Oceanography:;2006:;Volume( 036 ):;issue: 001:;page 64
    Author(s): Kieke, Dagmar; Rhein, Monika; Stramma, Lothar; Smethie, William M.; LeBel, Deborah A.; Zenk, Walter
    Publisher: American Meteorological Society
    Abstract: Chlorofluorocarbon (component CFC-11) and hydrographic data from 1997, 1999, and 2001 are presented to track the large-scale spreading of the Upper Labrador Sea Water (ULSW) in the subpolar gyre of the North Atlantic Ocean. ...
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    Decadal Changes in Water Mass Characteristics at 24°N in the Subtropical North Atlantic Ocean 

    Source: Journal of Climate:;1996:;volume( 009 ):;issue: 012:;page 3162
    Author(s): Bryden, Harry L.; Griffiths, Michael J.; Lavin, Alicia M.; Millard, Robert C.; Parrilla, Gregorio; Smethie, William M.
    Publisher: American Meteorological Society
    Abstract: Three transatlantic hydrographic sections across 24°N through the center of the subtropical gyre are analyzed for evidence of decadal changes in water mass characteristics. In the main thermocline, there has been a steady ...
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