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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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    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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    The Role of Meltwater Advection in the Formulation of Conservative Boundary Conditions at an Ice–Ocean Interface 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 001:;page 285
    Author(s): Jenkins, Adrian; Hellmer, Hartmut H.; Holland, David M.
    Publisher: American Meteorological Society
    Abstract: Upper boundary conditions for numerical models of the ocean are conventionally formulated under the premise that the boundary is a material surface. In the presence of an ice cover, such an assumption can lead to nonconservative ...
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    A Rossby Wave Bridge from the Tropical Atlantic to West Antarctica 

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 006:;page 2256
    Author(s): Li, Xichen; Gerber, Edwin P.; Holland, David M.; Yoo, Changhyun
    Publisher: American Meteorological Society
    Abstract: ropical Atlantic sea surface temperature changes have recently been linked to circulation anomalies around Antarctica during austral winter. Warming in the tropical Atlantic associated with the Atlantic multidecadal ...
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