The origin of a slowly varying irradiance component may derive from changes in
the solar faculae and / or in the background solar radiation from solar quiet regions.
Not exact matches
Because of the variations of sunspots and
faculae on the sun's surface, the total
solar irradiance (TSI), also called the
solar constant, varies on a roughly 11 - year cycle by about 0.07 %, which has been measured by orbiting satellites since 1978 [Lean, 1987, 1991; Wilson et al., 1981].
Foukal point out correctly that the arguments used for supporting a long term
solar component — other than that related to sunspot /
faculae — have fallen down.
This increase has not been measured by the other satellite measuring at this period (ERBS); b) other indicators of
solar activity, which are closely correlated to TSI (sunspot number,
faculae, geomagnetic activity) show no trend in that period, either.
Since the
solar UV irradiance has no long - term trend, the mechanism for the secular change of TSI must differ from the effect of surface magnetism, as manifested by sunspots,
faculae, and network which indeed explain well the intra-cycle variability of both total and spectral irradiance.
That jibes with the idea of a cooling trend during
solar minimum; fewer spots means fewer
faculae, so the Sun emits less Earth - warming radiation.
Sunspots are surrounded by a rim called
faculae, and in this region the temperatures are actually higher than the average
solar surface.
In this study, we address the question of whether the observed decrease in the TSI is the result of evolving
solar surface magnetism (sunspots and
faculae).
Key words: methods: data analysis /
solar - terrestrial relations / Sun: activity / Sun:
faculae, plages / Sun: magnetic fields / sunspots
We use a TSI model that is solely based on
solar surface magnetic phenomena (sunspots and
faculae including network).
Because our main goal is to reproduce the centennial
solar variability and because magnetograms are unavailable for historical time periods, we scale the
faculae and the active network filling factors with the sunspot number instead of using filling factors derived from available magnetogram data.
One explanation for the postulated reduction in
solar radiation during the 17th century Maunder Minimum is that the Sun's surface was not only largely devoid of spots and
faculae, but also less bright, overall.
Key words: Sun:
solar - terrestrial relations / methods: data analysis / Sun: activity / Sun:
faculae, plages / Sun: magnetic fields / Sun: sunspots
In years of maximum
solar activity, it is the bright
faculae that prevail, raising the levels of both total and UV radiation.