When mass balance, surface temperature and geothermal input are known, the mean ice temperature at the grounding line can be obtained as a residual. The procedure is applied to the drainage basin feeding the Ross Ice Shelf. -from Current Antarctic Literature
CITATION STYLE
Oerlemans, J. (1987). Heat budget of the Ross drainage basin. Dyamics of the West Antarctic Ice Sheet, 287–292. https://doi.org/10.1007/978-94-009-3745-1_15
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