Simulation and inversion of borehole temperature profiles in surrogate climates: Spatial distribution and surface coupling
A heat‐conduction forward model driven by ground surface temperature from three 1000‐year climate simulations with the state‐of‐the‐art ECHO‐g model has been used to simulate underground temperature perturbation profiles. An inversion approach has been applied to reconstruct ground surface temperatu...
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Veröffentlicht in: | Geophysical research letters 2006-01, Vol.33 (1), p.n/a |
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Sprache: | eng |
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