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ko value for southeastern Utah compensates for the increased variability of thermal conductivities (and other thermophysical rock properties) associated with the layered sedimentary strata in which these temperature-depth measurements were made.
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ko value for southeastern Utah compensates for the increased variability of thermal conductivities (and other thermophysical rock properties) associated with the layered sedimentary strata in which these temperature-depth measurements were made.
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84920296880
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in preparation
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_, in preparation.
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21
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0030512020
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Averaging solutions is equivalent to a simultaneous inversion and enhances the long-period signal of regional climate change [H. N. Pollack, P. Y. Shen, S. Huang, Pure Appl. Geophys. 147, 537 (1996)].
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Stations comprising the HCN have the properties of a relatively long temperature series, a predominantly undisturbed environment around the meteorological site, and limited station relocations [D. R. Easterling, T. R. Karl, E. H. Mason, P. Y. Hughes, D. P. Bowman, United States Historical Climatology Network (U.S. HCN) Monthly Temperature and Precipitation Data. ORNL/CDIAC-87, NDP-019/R3 (Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, Oak Ridge, TN, 1996)].
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Bowman, D.P.5
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84920296879
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note
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We thank A. H. Lachenbruch, whose early work on climate reconstruction from borehole temperatures stimulated parts of this study, for providing constructive comments. Supported by the National Science Foundation (EAR-9104292 and EAR-9205031) and grant project No. 92037 of the Czech-U.S. Science and Technology Cooperation Program.
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