The dynamic loss of ice via outlet glaciers around the Greenland Ice Sheet is a major contributor to sea level rise. However, the retreat history and ensuing dynamic mass loss of neighboring glaciers are disparate, complicating Here, we examine the evolution for three neighboring glaciers prior to; at the onset of; during; and, where possible, after retreat. in lateral drag and associated glacier acceleration. may control retreat duration and thus the long-term dynamic response of a glacier to terminus retreat. Specifically, glaciers with large regions of extending far inland from the terminus permit a chain of stress changes that results in sustained acceleration, increased mass loss, and continued retreat into the future despite a pause in ocean forcing.
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Answer:
Rate of change of velovity is called a acceleration.
Explanation:
Vf-Vi
t
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Answer:
The dynamic loss of ice via outlet glaciers around the Greenland Ice Sheet is a major contributor to sea level rise. However, the retreat history and ensuing dynamic mass loss of neighboring glaciers are disparate, complicating Here, we examine the evolution for three neighboring glaciers prior to; at the onset of; during; and, where possible, after retreat. in lateral drag and associated glacier acceleration. may control retreat duration and thus the long-term dynamic response of a glacier to terminus retreat. Specifically, glaciers with large regions of extending far inland from the terminus permit a chain of stress changes that results in sustained acceleration, increased mass loss, and continued retreat into the future despite a pause in ocean forcing.