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@article{
 title = {Description of a hybrid ice sheet-shelf model, and application to Antarctica},
 type = {article},
 year = {2012},
 pages = {1273-1295},
 volume = {5},
 websites = {http://www.geosci-model-dev.net/5/1273/2012/gmd-5-1273-2012.pdf},
 publisher = {gmd-5-1273-2012},
 id = {b346e6b4-c01b-3b89-9033-72f43af15ce6},
 created = {2015-11-11T17:16:22.000Z},
 file_attached = {false},
 profile_id = {58d47d98-a4f4-3ac1-a79d-2d252a797376},
 group_id = {2ba26f0d-672d-3e62-890c-74a17b5168fd},
 last_modified = {2017-03-14T13:27:08.137Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {pollard2012description},
 source_type = {misc},
 private_publication = {false},
 abstract = {The formulation of a 3-D ice sheet-shelf model is described. The model is designed for long-term continentalscale applications, and has been used mostly in paleoclimatic studies. It uses a hybrid combination of the scaled shallow ice and shallow shelf approximations for ice flow. Floating ice shelves and grounding-line migration are included, with parameterized ice fluxes at grounding lines that allows relatively coarse resolutions to be used. All signifi- cant components and parameterizations of the model are described in some detail. Basic results for modern Antarctica are compared with observations, and simulations over the last 5 million years are compared with previously published results. The sensitivity of ice volumes during the last deglaciation to basal sliding coefficients is discussed.},
 bibtype = {article},
 author = {Pollard, D and DeConto, R M},
 doi = {10.5194/gmd-5-1273-2012},
 journal = {Geosci. Model Dev.}
}