Global map of solid Earth surface heat flow

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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 .”