1201.2539 (C. Karoff)
C. Karoff
The integrated brightness of the Sun shows variability on time-scales from
minutes to decades. This variability is mainly caused by pressure mode
oscillations, by granulation and by dark spots and bright faculae on the
surface of the Sun. By analyzing the frequency spectrum of the integrated
brightness we can obtain greater knowledge about these phenomena. It is shown
how the frequency spectrum of the integrated brightness of the Sun in the
frequency range from 0.1 to 3.2 mHz shows clear signs of both granulation,
faculae and p-mode oscillations and that the measured characteristic
time-scales and amplitudes of the acoustic signals from granulation and faculae
are consistent with high-resolution observations of the solar surface. Using 13
years of observations of the Sun's integrated brightness from the VIRGO
instrument on the SOHO satellite it is shown that the significance of the
facular component varies with time and that it has a significance above 0.99
around half the time. Furthermore, an analysis of the temporal variability in
the measured amplitudes of both the granulation, faculae and p-mode oscillation
components in the frequency spectrum reveals that the amplitude of the p-mode
oscillation component shows variability that follows the solar cycles, while
the amplitudes of the granulation and facular components show signs of
quasi-annual and quasi-biennial variability, respectively.
View original:
http://arxiv.org/abs/1201.2539
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