Tidal and spatial variability of flow speed and seismicity near the grounding zone of Beardmore Glacier, Antarctica
GPS measurements of tidal modulation of ice flow and seismicity within the grounding zone of Beardmore Glacier show that tidally induced fluctuations of horizontal flow are largest near the grounding line and decrease downstream. Seismic activity is continuous, but peaks occur on falling and rising...
Main Authors: | , , , |
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Format: | Text |
Language: | unknown |
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ScholarWorks@CWU
2019
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Online Access: | https://digitalcommons.cwu.edu/cotsfac/104 https://digitalcommons.cwu.edu/cgi/viewcontent.cgi?article=1104&context=cotsfac |