2009
DOI: 10.1017/s1743921309992687
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Mechanisms for total and spectral solar irradiance variations

Abstract: Abstract. The total and spectral irradiance varies over short time scales, i.e. from days to months, and longer time scales from years to decades, centuries, and beyond. In this talk we review the current understanding of irradiance changes from days to decades. We present the current status of observations and discuss proposed reconstruction approaches to understand these variations. The main question that ultimately needs to be answered is what are the physical processes that could explain the enhanced heati… Show more

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Cited by 3 publications
(4 citation statements)
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References 43 publications
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“…Most of the chromospheric emission lines formed at temperatures below 2 × 10 4 K are emitted by chromospheric ions (Doschek et al 1977). The main chromospheric emission lines for the 0.5 nm wavelength interval in the range 200.5 nm -300.5 nm are C II, Co II, Cr II, Fe II, Mg II h&k line, Mn II, Ni II and Ti II, and all these emission lines are a function of wavelength (Haberreiter 2010).…”
Section: Data Analysis Resultsmentioning
confidence: 96%
“…Most of the chromospheric emission lines formed at temperatures below 2 × 10 4 K are emitted by chromospheric ions (Doschek et al 1977). The main chromospheric emission lines for the 0.5 nm wavelength interval in the range 200.5 nm -300.5 nm are C II, Co II, Cr II, Fe II, Mg II h&k line, Mn II, Ni II and Ti II, and all these emission lines are a function of wavelength (Haberreiter 2010).…”
Section: Data Analysis Resultsmentioning
confidence: 96%
“…A range of other spectral activity indicators have also been explored and found useful as tracers of chromospheric magnetic activity (see Figure 6), flares and plages, including Hα [4,110] and Hβ emission [111], He I D 3 (587.59 nm) and 1.08 µm absorption [112][113][114][115], the Na I D 1 and D 2 lines, the infrared Ca II triplet absorption lines (centred at 8498.062 Å, 8542.144 Å and 8662.170 Å), and extreme ultraviolet (UV; 200.5-300.5 nm) resonance lines associated with surface effective temperatures T eff < 2 × 10 4 K, including C I, C II, Co II, Cr II, Fe II, Mn II, Ni II, O I, Si II and Ti II [116], as well as Mg II h and k [117][118][119]. Of these, Fe II (298.5 nm) is the dominant contributor to solar irradiance variations in high-ionisation environments [114].…”
Section: Spectroscopic Diagnosticsmentioning
confidence: 99%
“…The second is daily sunspot area of the full Sun. Sunspot area is sometimes used to represent "the sunspots blocking" [11,37], which can be downloaded from NASA (https://solarscience.msfc.nasa.gov/greenwch.shtml). The third is Mg II core-to-wing ratio, called Mg II index in this study, which is a robust measure of chromospheric activity [38][39][40].…”
Section: The Reason For the Solar Cycle Variation Of Tsimentioning
confidence: 99%
“…The variability of the photosphere (wings) is quite small, while the chromospheric activity causes about 30% variations of the core. Because the core-to-wing ratio is not easily affected by the instruments, Mg II index which is used to represent "the intensification due to bright faculae, plages, and network elements" is very reliable [11,37,38]. The Mg II index composite can be downloaded from the website http://www .iup.uni-bremen.de/gome/gomemgii.html.…”
Section: The Reason For the Solar Cycle Variation Of Tsimentioning
confidence: 99%