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Table 1 Estimates of thermal effects of processes not modeled in Syracuse et al. (2010)

From: An introductory review of the thermal structure of subduction zones: III—Comparison between models and observations

Effect

Impact

Temperature difference

Primary

Melt migration

Local

Few 100\(^\circ\)C

Backarc spreading

Local and shallow

Few 100\(^\circ\)C

Time-dependence of forcing parameters

Global

100–200\(^\circ\)C

3D flow effects

Global

100–200\(^\circ\)C

Rheology of the mantle wedge

Global

??

Variable radiogenic heating

Local

\(\sim\)50–100\(^\circ\)C

Decoupling-coupling transition

Local

Could be large locally

Secondary

Fluid flow in slab

Local to shallow slab

10–50\(^\circ\)C

Shear heating

Local to seismogenic zone

50–100\(^\circ\)C

Phase changes

Local to shallow slab

50\(^\circ\)C