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    Observation of a Bathymetrically Trapped Current Ring 

    Source: Journal of Physical Oceanography:;1977:;Volume( 007 ):;issue: 006:;page 946
    Author(s): Kinder, T. H.; Coachman, L. K.
    Publisher: American Meteorological Society
    Abstract: Examination of hydrographic data obtained over a large submarine canyon revealed a cell with a core of high salinity water nestled in the outer (deeper) reaches of the canyon. Bemuse of the T-S distribution within the cell ...
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    On Lateral Water Mass Interaction—A Case Study, Bristol Bay, Alaska 

    Source: Journal of Physical Oceanography:;1979:;Volume( 009 ):;issue: 002:;page 278
    Author(s): Coachman, L. K.; Charnell, R. L.
    Publisher: American Meteorological Society
    Abstract: Salinity-temperature-depth data obtained on several spring and summer cruises during 1976 and 1977 from outer Bristol Bay in the southeast Bering Sea indicate the existence of a zone, between two well-defined water masses, ...
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    Circulation Patterns Near the Tail of the Grand Banks 

    Source: Journal of Physical Oceanography:;1973:;Volume( 003 ):;issue: 004:;page 397
    Author(s): Voorheis, G. M.; Aagaard, K.; Coachman, L. K.
    Publisher: American Meteorological Society
    Abstract: Dynamic topographies for the region surrounding the tail of the Grand Banks have been examined for the years 1922?65, in an attempt to define the characteristics of the eddies and meanders typical of the circulation pattern. ...
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    On the Flow Through Barrow Canyon 

    Source: Journal of Physical Oceanography:;1976:;Volume( 006 ):;issue: 004:;page 461
    Author(s): Mountain, David G.; Coachman, L. K.; Aagaard, Knut
    Publisher: American Meteorological Society
    Abstract: Simultaneous current and temperature measurements were made at two depths in Barrow Canyon for a period of 120 days from April through August, 1973. The mean of the measured currents was 25 cm s?1 toward the northeast, ...
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    The Bering Slope Current System 

    Source: Journal of Physical Oceanography:;1975:;Volume( 005 ):;issue: 002:;page 231
    Author(s): Kinder, T. H.; Coachman, L. K.; Galt, J. A.
    Publisher: American Meteorological Society
    Abstract: The Bering Slope Current flows from southeast to northwest across the Aleutian Basin of the Bering Sea, parallel to the continental slope of the eastern Bering Sea shelf. The water mass characteristics and distributions ...
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