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Table 3
Radiative-equilibrium (RE) temperatures at slab center and at its surface (in parentheses).
| p [dyne cm-2] | 0.01 | 0.1 | 0.5 | Model |
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| D = 200 km | 9750 (9760) | 7990 (8180) | 7010 (7560) | HI only |
| D = 1000 km | 9700 (9710) | 7400 (8050) | 6620 (7550) | |
| D = 5000 km | 9480 (9570) | 6780 (8020) | 6340 (7550) | |
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| D = 200 km | 9530 (9530) | 6770 (7270) | 5040 (6030) | HI + Ca ii (updated) |
| D = 1000 km | 9470 (9480) | 5460 (7030) | 4690 (6010) | |
| D = 5000 km | 9200 (9300) | 4960 (7000) | 4360 (5990) | |
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| D = 200 km | 8280 (8280) | 6080 (6530) | 4960 (5720) | HI, Ca ii + Mg ii |
| D = 1000 km | 8140 (8190) | 5260 (6370) | 4680 (5710) | |
| D = 5000 km | 7650 (7920) | 4880 (6360) | 4430 (5690) | |
Notes.Three sets of models are shown: RE only with hydrogen losses, RE with hydrogen and Ca ii losses, and RE with Mg ii losses added.
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