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Deep soil temperature as proxy for surface air‐temperature in a coupled model simulation of the last thousand years

González‐Rouco, F., von Storch, H., Zorita, E.·2003·Geophysical Research Letters

Abstract

The relationship between terrestrial deep soil temperature (TDST) and surface temperature (SAT) at interannual and centennial timescales has been investigated in a simulation of the last millennium with a three‐dimensional climate model driven by estimations of historical external forcing. TDST is loosely related to borehole temperature profiles, which have been recently used to reconstruct long term temperature trends in the last centuries. Recently, questions about the validity of boreholes‐based reconstructions have been raised. In the simulation, at interannual time scales the connection between TDST and SAT is stable, being stronger in the summer half year than in the winter half year. At long timescales, annual TDSL is a good proxy for annual SAT, and their variations are almost indistinguishable from each other. Both TDSL and terrestrial SAT overestimate the variations of global mean SAT. This may be a source for the disagreement between statistical reconstructions of global SAT and terrestrial borehole measurements.

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Metadata

Authors
González‐Rouco, F., von Storch, H., & Zorita, E.
Venue
Geophysical Research Letters
Published
2003-11
Volume
30
Issue
21
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2048485366
Cited by
190
References
0
FWCI
17.99
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Deep soil temperature as proxy for surface air‐temperature in a coupled model simulation of the last thousand years. https://app.cochat.ai/papers/10.1029/2003gl018264
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González‐Rouco, F., von Storch, H., & Zorita, E. (2003). Deep soil temperature as proxy for surface air‐temperature in a coupled model simulation of the last thousand years. Geophysical Research Letters. https://doi.org/10.1029/2003gl018264

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