Vertical Strain at Siple Dome, Antarctica, 1999-2002
Abstract: At the Siple Dome area of Antarctica, much of the ice flow is vertical, which causes vertical ice deformation. To measure this phenomenon, the investigators used a method known as vertical strain rate. This project was a part of the West Antarctic Ice Sheet Cores (WAISCORES) project for de...
Main Authors: | , , , , , |
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Format: | Dataset |
Language: | unknown |
Published: |
IEDA: US Antarctic Program Data Center
2007
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Subjects: | |
Online Access: | http://get.iedadata.org/metadata/iso/609214 |