Global map of solid Earth surface heat flow
By J. Huw Davies. 2013
318 citations recorded by the source corpus.
Subfields: Atmospheric Science, Geophysics, Mechanics of Materials
View Paper: https://www.semanticscholar.org/paper/eacdb7e6c888a058e8eadcb520040a320f338b61
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In Atmospheric Science
- Robert Hallberg
- S. Griffies
- Andrew T. Wittenberg
- I. Held
- Alistair Adcroft
- M. Harrison
- Malte Jansen
- M. Winton
In Geophysics
In Mechanics of Materials
Citations in the corpus
- Analysis and Mapping of an Updated Terrestrial Heat Flow Data Set (2019, methodology): “The most commonly used predictors are geology (Lee, 1965) and age (Chapman & Pollack, 1975); recent analysis using them include Davies and Davies (2010) and Davies (2013), while Artemieva (2006) exclusively used them for continents.”
- The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features (2019, methodology): “(2010). Operationally, this scheme is implemented as an interface height diffusion to avoid problems with layer thickness diffusion described by Holloway (1997). Furthermore, we apply the associated eddy induced transport via a bolus velocity as commonly used in layer models (e.”
- Lifetime and size of shallow magma bodies controlled by crustal-scale magmatism (2017, unknown): “The surface temperature is set at 0 ° C and mantle heat flux is fixed at 40 mW/m 2 , corresponding to ~75 mW/m 2 initial surface heat flow, consistent with the average heat flow of crust of the modern Earth in different settings 54-56 .”