TY - JOUR
T1 - Ice streams - Fast, and faster?
AU - Alley, Richard B.
AU - Anandakrishnan, Sridhar
AU - Dupont, Todd K.
AU - Parizek, Byron R.
N1 - Funding Information:
We thank numerous colleagues in the West Antarctic Ice Sheet Project, the West Antarctic Ice Cores Project and elsewhere for ideas and discussions, Ian Joughin for the base data in Fig. 2, Paul Duval and Jerome Weiss for helpful suggestions on the manuscript, and the National Science Foundation Office of Polar Programs for funding through grants including 0126187, 0229629 and 9814774; partial funding also was provided by the G. Comer Foundation.
PY - 2004/9
Y1 - 2004/9
N2 - Rapid flow of ice streams is caused either by great thickness, or by effective basal lubrication especially from deforming tills. Competing thermal processes act to stabilize and to destabilize the well-lubricated ice streams, and may contribute to their observed short-term variability yet long-term persistence. Increasing evidence indicates that ice streams are subject to speed-up in response to warming, through thinning or loss of ice shelves, and possibly in response to meltwater penetration to ice-stream beds.
AB - Rapid flow of ice streams is caused either by great thickness, or by effective basal lubrication especially from deforming tills. Competing thermal processes act to stabilize and to destabilize the well-lubricated ice streams, and may contribute to their observed short-term variability yet long-term persistence. Increasing evidence indicates that ice streams are subject to speed-up in response to warming, through thinning or loss of ice shelves, and possibly in response to meltwater penetration to ice-stream beds.
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U2 - 10.1016/j.crhy.2004.08.002
DO - 10.1016/j.crhy.2004.08.002
M3 - Short survey
AN - SCOPUS:9144228299
SN - 1631-0705
VL - 5
SP - 723
EP - 734
JO - Comptes Rendus Physique
JF - Comptes Rendus Physique
IS - 7
ER -