Repeat temperature measurements in borehole GC-1, northwestern Utah: towards isolating a climate-change signal borehole temperature profiles

Citeable URL: https://ir.library.oregonstate.edu/concern/articles/z603qz95r

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Attribute Name	Values
Creator	Chapman, David S. Harris, Robert N.
Abstract	Temperature-depth profiles in borehole CC-I, northwestern Utah, were measured in 1978, 1990, and 1992. Borehole temperatures below 80 m depth are highly reproducible over the 14 year period indicating long term thermal stability. A slowly changing temperature field above 80 m depth has similiar characteristics to synthetic temperature profiles computed from a 100 year record of air temperature changes at Park Valley weather station 50 km northeast of the borehole site.
Resource Type	Article
DOI	https://doi.org/10.1029/93GL01877
Date Available	2010-04-22T21:07:19+00:00
Date Issued	1993-09-15
Citation	Chapman, David S., and Robert N. Harris. "Repeat temperature measurements in borehole GC-1, northwestern Utah: towards isolating a climate-change signal borehole temperature profiles." Geophysical Research Letters 20.18 (1993): 1891-94. Print.
Journal Title	Geophysical Research Letters
Journal Volume	20
Journal Issue/Number	18
Rights Statement	In Copyright
Publisher	American Geophysical Union
Language	English [eng]
Replaces	http://hdl.handle.net/1957/15632

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