Articles | Volume 12, issue 1
https://doi.org/10.5194/tc-12-49-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-12-49-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
09 Jan 2018
Research article |
| 09 Jan 2018
Modelling present-day basal melt rates for Antarctic ice shelves using a parametrization of buoyant meltwater plumes
Werner M. J. Lazeroms
CORRESPONDING AUTHOR
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, the Netherlands
Adrian Jenkins
British Antarctic Survey, Natural Environment Research Council, Cambridge, UK
G. Hilmar Gudmundsson
British Antarctic Survey, Natural Environment Research Council, Cambridge, UK
Roderik S. W. van de Wal
Institute for Marine and Atmospheric Research Utrecht, Utrecht University, Utrecht, the Netherlands
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- A framework for estimating the anthropogenic part of Antarctica’s sea level contribution in a synthetic setting A. Bradley et al. 10.1038/s43247-024-01287-w
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- Sensitivity of the future evolution of the Wilkes Subglacial Basin ice sheet to grounding-line melt parameterizations Y. Wang et al. 10.5194/tc-18-5117-2024
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5 citations as recorded by crossref.
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- Ocean‐Forced Ice‐Shelf Thinning in a Synchronously Coupled Ice‐Ocean Model J. Jordan et al. 10.1002/2017JC013251
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Short summary
Basal melting of ice shelves is a major factor in the decline of the Antarctic Ice Sheet, which can contribute significantly to sea-level rise. Here, we investigate a new basal melt model based on the dynamics of meltwater plumes. For the first time, this model is applied to all Antarctic ice shelves. The model results in a realistic melt-rate pattern given suitable data for the topography and ocean temperature, making it a promising tool for future simulations of the Antarctic Ice Sheet.
Basal melting of ice shelves is a major factor in the decline of the Antarctic Ice Sheet, which...
