Abstract
Ice shelves are the floating extensions of ice sheets into the ocean. Melting under ice shelves contributes to their mass balance and affects their geometry, with implications for ice-shelf evolution and integrity. This chapter examines the relevant ice-ocean interactions, focussing on mathematical descriptions of the plume dynamics that control the basal melt rate, and of the large-scale ocean circulation in the sub ice-shelf cavities.
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Notes
- 1.
At sufficiently low concentrations, the phase change occurs close to 0 °C and ‘melting’ is the appropriate term. We use this term from now on to describe melting and dissolution, as their distinction is not critical to the discussion.
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Jenkins, A. (2021). Interaction of Ice Shelves with the Ocean. In: Fowler, A., Ng, F. (eds) Glaciers and Ice Sheets in the Climate System. Springer Textbooks in Earth Sciences, Geography and Environment. Springer, Cham. https://doi.org/10.1007/978-3-030-42584-5_5
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