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Solar facula
Photospheric phenomenon From Wikipedia, the free encyclopedia
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Solar faculae are bright spots in the photosphere that form in the canyons between solar granules, short-lived convection cells several thousand kilometers across that constantly form and dissipate over timescales of several minutes.
![]() | This article's factual accuracy is disputed. (December 2023) |

Faculae are produced by concentrations of magnetic field lines. Strong concentrations of faculae appear during increased solar activity, with or without sunspots. Faculae and sunspots contribute noticeably to variations in the solar constant. The chromospheric counterpart of a facular region is called a plage.[1][2][3][4]
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