TY - JOUR
T1 - Rapid dynamic activation of a marine-based Arctic ice cap
T2 - Ice cap dynamic activation
AU - Mcmillan, Malcolm
AU - Shepherd, Andrew
AU - Gourmelen, Noel
AU - Dehecq, Amaury
AU - Leeson, Amber
AU - Ridout, Andrew
AU - Flament, Thomas
AU - Hogg, Anna
AU - Gilbert, Lin
AU - Benham, Toby
AU - Van Den Broeke, Michiel
AU - Dowdeswell, Julian A.
AU - Fettweis, Xavier
AU - No??l, Brice
AU - Strozzi, Tazio
PY - 2015/1/27
Y1 - 2015/1/27
N2 - We use satellite observations to document rapid acceleration and ice loss from a formerly slow-flowing, marine-based sector of Austfonna, the largest ice cap in the Eurasian Arctic. During the past two decades, the sector ice discharge has increased 45-fold, the velocity regime has switched from predominantly slow (~ 101 m/yr) to fast (~ 103 m/yr) flow, and rates of ice thinning have exceeded 25 m/yr. At the time of widespread dynamic activation, parts of the terminus may have been near floatation. Subsequently, the imbalance has propagated 50 km inland to within 8 km of the ice cap summit. Our observations demonstrate the ability of slow-flowing ice to mobilize and quickly transmit the dynamic imbalance inland; a process that we show has initiated rapid ice loss to the ocean and redistribution of ice mass to locations more susceptible to melt, yet which remains poorly understood.
AB - We use satellite observations to document rapid acceleration and ice loss from a formerly slow-flowing, marine-based sector of Austfonna, the largest ice cap in the Eurasian Arctic. During the past two decades, the sector ice discharge has increased 45-fold, the velocity regime has switched from predominantly slow (~ 101 m/yr) to fast (~ 103 m/yr) flow, and rates of ice thinning have exceeded 25 m/yr. At the time of widespread dynamic activation, parts of the terminus may have been near floatation. Subsequently, the imbalance has propagated 50 km inland to within 8 km of the ice cap summit. Our observations demonstrate the ability of slow-flowing ice to mobilize and quickly transmit the dynamic imbalance inland; a process that we show has initiated rapid ice loss to the ocean and redistribution of ice mass to locations more susceptible to melt, yet which remains poorly understood.
U2 - 10.1002/2014GL062255
DO - 10.1002/2014GL062255
M3 - Article
SN - 0094-8276
VL - 41
SP - 8902
EP - 8909
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 24
ER -