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Vertical Strain at Siple Dome, Antarctica, 1999-2002 Data DOI: https://doi.org/10.7265/N5HH6H00 Cite as Harrison, W., Elsberg, D., Morack, J., Pettit, E. C., Waddington, E. D., & Zumberge, M. (2007) "Vertical Strain at Siple Dome, Antarctica, 1999-2002" U.S. Antarctic Program (USAP) Data Center. doi: https://doi.org/10.7265/N5HH6H00. AMD - DIF Record(s) NSIDC-0214_1 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 deep ice coring in West Antarctica. WAISCORES is supported by the Office of Polar Programs (OPP), National Science Foundation (NSF). This data set consists of a table of long-term average strain rates measured between 1999 and 2002 at Siple Dome, Antarctica. The measurements were taken in hot-water boreholes by bridge gauges. Data are available in tab-delimited ASCII text format or PDF via FTP. Creator(s): Harrison, William Date Created: 2007-02-22 Repository: USAP-DC (current) - NSIDC (original) License: Creative Commons Attribution-NonCommercial v4.0 Generic [CC BY-NC 4.0] Spatial Extent(s) West: -148.822, East: -148.822, South: -81.655, North: -81.655 West: -148.693, East: -148.693, South: -81.595, North: -81.595 Temporal Extent(s) Start: 1999-12-05 - End: 2002-01-02 Award(s) NSF 9615502 Version: 1 Related Project(s) Ice Dynamics, the Flow Law, and Vertical Strain at Siple Dome References Elsberg, D. H., W. D. Harrison, E. Husmann, J. L. Morack, E. C. Pettit, E. D. Waddington, and M. A. Zumberge. 2004. Depth- and time-dependent strain rates at Siple Dome, Antarctica. Journal of Glaciology 50 (171): 511-521. (doi:10.3189/172756504781829684) Keywords Antarctica Geodesy Geology/Geophysics - Other Glaciers/ice Sheet Glaciology Siple Dome Siple Dome Ice Core Strain WAISCORES