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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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    The Fate of the Southern Weddell Sea Continental Shelf in a Warming Climate 

    Source: Journal of Climate:;2017:;volume( 030 ):;issue: 012:;page 4337
    Author(s): Hellmer, Hartmut H.; Kauker, Frank; Timmermann, Ralph; Hattermann, Tore
    Publisher: American Meteorological Society
    Abstract: arm water of open ocean origin on the continental shelf of the Amundsen and Bellingshausen Seas causes the highest basal melt rates reported for Antarctic ice shelves with severe consequences for the ice shelf/ice sheet ...
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    Future Projections of Antarctic Ice Shelf Melting Based on CMIP5 Scenarios 

    Source: Journal of Climate:;2018:;volume 031:;issue 013:;page 5243
    Author(s): Naughten, Kaitlin A.; Meissner, Katrin J.; Galton-Fenzi, Benjamin K.; England, Matthew H.; Timmermann, Ralph; Hellmer, Hartmut H.
    Publisher: American Meteorological Society
    Abstract: AbstractBasal melting of Antarctic ice shelves is expected to increase during the twenty-first century as the ocean warms, which will have consequences for ice sheet stability and global sea level rise. Here we present ...
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