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- W150660682 abstract "The time levels are chosen to represent the evolution of the event. • after 300 yrs, the event sets in. • after 1000 yrs, most of the ice has run out. • after 3000 yrs, the event in the run with basal water advection has terminated. The other two never do. With 0.1 m of basal water as limit, the ice sheet fails to loose sufficient amounts of ice to return to a calm state and ends up with a quick succession of pulses from different areas that appear as a constant stream. With 10 m of basal water as limit, the Hudson Strait does not refreeze since the heat storage capacity of the basal water is too large. With unlimited basal water and basal water advection, in the earlier parts of the event, ice with high basal water amounts is advected into the strait and the basal water level rises. Then, as the surge weakens, the ice advected into the strait brings less basal water and the basal water level decreases again so the surge can terminate." @default.
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- W150660682 date "2010-05-01" @default.
- W150660682 modified "2023-09-23" @default.
- W150660682 title "Laurentide Ice Sheet surging as modeled with PISM" @default.
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