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    Recent Observations of Variability in the Path and Vertical Structure of the Alaskan Stream 

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 010:;page 1634
    Author(s): Reed, Ronald K.; Stabeno, Phyllis J.
    Publisher: American Meteorological Society
    Abstract: Current records were recently obtained from two sites on the Continental slope southwest of Kodiak Island. At the inshore site (10-month record), flow mainly resembled the weak shelf-break flow typical of the Gulf of Alaska. ...
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    Mixing and Intrusions in a Rotating Cold-Core Feature off Cape Blanco, Oregon 

    Source: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 006:;page 823
    Author(s): Moum, James N.; Caldwell, Douglas R.; Stabeno, Phyllis J.
    Publisher: American Meteorological Society
    Abstract: During August 1986, a large cold anomaly was observed in satellite and in situ measurements near Cape Blanco at 42°N, 126°30?W off the Pacific Coast. Detailed vertical profiles of temperature, conductivity, turbulent ...
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    The Bering Slope Current System Revisited 

    Source: Journal of Physical Oceanography:;2004:;Volume( 034 ):;issue: 002:;page 384
    Author(s): Johnson, Gregory C.; Stabeno, Phyllis J.; Riser, Stephen C.
    Publisher: American Meteorological Society
    Abstract: Mean circulation and water properties within the Aleutian Basin of the Bering Sea are investigated using hydrographic and subsurface park pressure displacement data from a regional array of 14 profiling CTD floats. After ...
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    Results of the First Arctic Heat Open Science Experiment 

    Source: Bulletin of the American Meteorological Society:;2017:;volume 099:;issue 003:;page 513
    Author(s): Wood, Kevin R.; Jayne, Steven R.; Mordy, Calvin W.; Bond, Nicholas; Overland, James E.; Ladd, Carol; Stabeno, Phyllis J.; Ekholm, Alexander K.; Robbins, Pelle E.; Schreck, Mary-Beth; Heim, Rebecca; Intrieri, Janet
    Publisher: American Meteorological Society
    Abstract: AbstractSeasonally ice-covered marginal seas are among the most difficult regions in the Arctic to study. Physical constraints imposed by the variable presence of sea ice in all stages of growth and melt make the upper ...
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