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    A Numerical Method for Solving the Forced Baroclinic Coastal-Trapped Wave Problem of General Form 

    Source: Journal of Atmospheric and Oceanic Technology:;1987:;volume( 004 ):;issue: 001:;page 220
    Author(s): Webster, Ian; Holland, David
    Publisher: American Meteorological Society
    Abstract: The determination of baroclinic coastal-trapped wave modes reduces to an eigenvalue problem quadratic in the eigenvalue if the long-wave assumption is not made. This problem can be expressed as a linear eigenvalue problem ...
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    An Impact of Subgrid-Scale Ice–Ocean Dynamics on Sea-Ice Cover 

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 007:;page 1585
    Author(s): Holland, David M.
    Publisher: American Meteorological Society
    Abstract: A coupled sea-ice?ocean numerical model is used to study the impact of an ill-resolved subgrid-scale sea-ice?ocean dynamical process on the areal coverage of the sea-ice field. The process of interest is the transmission ...
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    Calving Signature in Ocean Waves at Helheim Glacier and Sermilik Fjord, East Greenland 

    Source: Journal of Physical Oceanography:;2016:;Volume( 046 ):;issue: 010:;page 2925
    Author(s): Vaňková, Irena; Holland, David M.
    Publisher: American Meteorological Society
    Abstract: hen glaciers calve icebergs, a fraction of the released potential energy is radiated away via gravity waves. The characteristics of such waves, caused by iceberg calving on Helheim Glacier in east Greenland, are investigated. ...
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    Adaptation of an Isopycnic Coordinate Ocean Model for the Study of Circulation beneath Ice Shelves 

    Source: Monthly Weather Review:;2001:;volume( 129 ):;issue: 008:;page 1905
    Author(s): Holland, David M.; Jenkins, Adrian
    Publisher: American Meteorological Society
    Abstract: Much of the Antarctic coastline comprises large, floating ice shelves, beneath which waters from the open ocean circulate. The interaction of the seawater with the base of these ice shelves has a bearing both on the rate ...
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    Modeling Thermodynamic Ice–Ocean Interactions at the Base of an Ice Shelf 

    Source: Journal of Physical Oceanography:;1999:;Volume( 029 ):;issue: 008:;page 1787
    Author(s): Holland, David M.; Jenkins, Adrian
    Publisher: American Meteorological Society
    Abstract: Models of ocean circulation beneath ice shelves are driven primarily by the heat and freshwater fluxes that are associated with phase changes at the ice?ocean boundary. Their behavior is therefore closely linked to the ...
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    Modeling Landfast Sea Ice by Adding Tensile Strength 

    Source: Journal of Physical Oceanography:;2010:;Volume( 040 ):;issue: 001:;page 185
    Author(s): König Beatty, Christof; Holland, David M.
    Publisher: American Meteorological Society
    Abstract: Landfast ice is sea ice that forms and remains fixed along a coast, where it is either attached to the shore or held between shoals or grounded icebergs. The current generation of sea ice models is not capable of reproducing ...
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    Instability and Mixing of Zonal Jets along an Idealized Continental Shelf Break 

    Source: Journal of Physical Oceanography:;2015:;Volume( 045 ):;issue: 009:;page 2315
    Author(s): Stern, Alon; Nadeau, Louis-Philippe; Holland, David
    Publisher: American Meteorological Society
    Abstract: he interaction between an Antarctic Circumpolar Current?like channel flow and a continental shelf break is considered using eddy-permitting simulations of a quasigeostrophic and a primitive equation model. The experimental ...
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    The Response of Ice Shelf Basal Melting to Variations in Ocean Temperature 

    Source: Journal of Climate:;2008:;volume( 021 ):;issue: 011:;page 2558
    Author(s): Holland, Paul R.; Jenkins, Adrian; Holland, David M.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional ocean general circulation model is used to study the response of idealized ice shelves to a series of ocean-warming scenarios. The model predicts that the total ice shelf basal melt increases quadratically ...
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    Oceanic Boundary Conditions for Jakobshavn Glacier. Part II: Provenance and Sources of Variability of Disko Bay and Ilulissat Icefjord Waters, 1990–2011 

    Source: Journal of Physical Oceanography:;2014:;Volume( 045 ):;issue: 001:;page 33
    Author(s): Gladish, Carl V.; Holland, David M.; Lee, Craig M.
    Publisher: American Meteorological Society
    Abstract: akobshavn Glacier, west Greenland, has responded to temperature changes in Ilulissat Icefjord, into which it terminates. Basin waters in this fjord exchange with neighboring Disko Bay waters of a particular density at least ...
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    Comparing Idealized and Complex Topographies in Quasigeostrophic Simulations of an Antarctic Circumpolar Current 

    Source: Journal of Physical Oceanography:;2013:;Volume( 043 ):;issue: 008:;page 1821
    Author(s): Nadeau, Louis-Philippe; Straub, David N.; Holland, David M.
    Publisher: American Meteorological Society
    Abstract: he circumpolar transport of a wind-driven quasigeostrophic Antarctic Circumpolar Current is considered. Simple theory suggests transport in a strongly forced regime?the focus of this study?is largely determined by a ...
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