Temperatures, Heat, and Energy in the Mantle of the Earth
By Claude Jaupart, Stéphane Labrosse, F. Lucazeau, J. Mareschal. 2007
260 citations recorded by the source corpus.
Subfields: Geophysics
View Paper: https://www.semanticscholar.org/paper/3f0136f7744119e94e796bb09852493b0141b78b
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In Geophysics
- J. Huw Davies
- Paul J. Tackley
- Jun Korenaga
- Frederic Deschamps
- Fabio Mantovani
- J. A. Connolly
- T. Nakagawa
- W. McDonough
Citations in the corpus
- Thermal evolution of the core with a high thermal conductivity (2014, unknown): “Clearly, large lateral variations of heat flux are expected at the CMB from mantle convection, as they are observed at the Earth surface (Jaupart et al., 2007), and for any reasonable value of the average CMB heat flux, we should expect regions of the CMB where the heat flux is super-isentropic and ”
- Mantle dynamics in super-Earths: Post-perovskite rheology and self-regulation of viscosity (2012, unknown): “…is generally thought that 342 heat from the core provides only a small fraction of the global heat budget (Davies and 343 k = ρCpκ κ =κ 0 ρ0 ρ ⎛ ⎝⎜ ⎞ ⎠⎟ −1 Richards, 1992; Jaupart et al., 2007; Schubert et al., 2000), therefore this is a reasonable first-344 order approximation to ignore it.”
- Global map of solid Earth surface heat flow (2013, background): “Such estimates continue to be refined and are agreeing at around 44–47 TW [Davies and Davies, 2010; Jaupart et al., 2007; © 2013.”
- The influence of MORB and harzburgite composition on thermo-chemical mantle convection in a 3-D spherical shell with self-consistently calculated mineral physics (2010, background): “…velocity during the last 2 billion years fluctuates from ∼2–6 cm/year and the surfaceheatflow is in the range20–25TW, the latter ofwhich is lower than the inferred Earth's present-day instantaneous surface heat flow of 46 TW (Jaupart et al., 2007), but this is a normal problem in evolution models.”
- Neutrino Physics with JUNO (2015, methodology): “For half a century we have established with considerable precision the Earthʼs surface heat flow as 46±3 TW [327, 328].”
- Urey ratio and the structure and evolution of Earth's mantle (2008, background): “, 1993] to 14 TW [Jaupart et al., 2007] on the basis of more recent heat flow”