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Modelling of the Fennoscandian Ice Sheet
1993The Fennoscandian ice sheet is simulated by means of a numerical model. The model includes three main parts: Ice flow mechanics (with the isothermal approximation), mass balance, and bedrock isostasy. The mass balance is based on the balance of atmospheric humidity, and takes into account the effect of orographically induced precipitation, which causes
Anne Letréguilly, Catherine Ritz
openaire +1 more source
Ice Sheet Initialization as an Integral Part of Ice sheet Modeling.
Proposed for presentation at the AGU Fall meeting 2021 in ,, 2021openaire +1 more source
Stability of the Antarctic Ice Sheet during the pre-industrial Holocene
Nature Reviews Earth & Environment, 2022Richard Jones +2 more
exaly
Modelling West Antarctic ice sheet growth and collapse through the past five million years
Nature, 2009David Pollard, Robert DeConto
exaly
Obliquity-paced Pliocene West Antarctic ice sheet oscillations
Nature, 2009David Harwood, David Pollard
exaly