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    Deep-Flow Variability at Drake Passage 

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 007:;page 1281
    Author(s): Klinck, John M.; Hofmann, Eileen E.
    Publisher: American Meteorological Society
    Abstract: A rotary empirical orthogonal function analysis of the currents measured in central Drake Passage during DRAKE 79 shows that the deep (2500 m) flow has the same spatial and temporal structure as the flow at 500 m, suggesting ...
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    Sensitivity of Circumpolar Deep Water Transport and Ice Shelf Basal Melt along the West Antarctic Peninsula to Changes in the Winds 

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 014:;page 4799
    Author(s): Dinniman, Michael S.; Klinck, John M.; Hofmann, Eileen E.
    Publisher: American Meteorological Society
    Abstract: ircumpolar Deep Water (CDW) can be found near the continental shelf break around most of Antarctica. Advection of this relatively warm water (up to 2°C) across the continental shelf to the base of floating ice shelves is ...
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    Effects of Projected Changes in Wind, Atmospheric Temperature, and Freshwater Inflow on the Ross Sea 

    Source: Journal of Climate:;2017:;volume 031:;issue 004:;page 1619
    Author(s): Dinniman, Michael S.; Klinck, John M.; Hofmann, Eileen E.; Smith, Walker O.
    Publisher: American Meteorological Society
    Abstract: AbstractA 5-km horizontal resolution regional ocean?sea ice?ice shelf model of the Ross Sea is used to examine the effects of changes in wind strength, air temperature, and increased meltwater input on the formation of ...
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