2015
DOI: 10.1051/swsc/2015013
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Identification of photospheric activity features from SOHO/MDI data using the ASAP tool

Abstract: The variation of solar irradiance is one of the natural forcing mechanisms of the terrestrial climate. Hence, the time-dependent solar irradiance is an important input parameter for climate modelling. The solar surface magnetic field is a powerful proxy for solar irradiance reconstruction. The analyses of data obtained with the Michelson Doppler Imager (MDI) on board the SOHO mission are therefore useful for the identification of solar surface magnetic features to be used in solar irradiance reconstruction mod… Show more

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Cited by 15 publications
(8 citation statements)
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“…The calculated filling factors for a feature reflect the fraction of the solar disk covered by the feature and assign reference synthetic spectra to it. [12] The filling factor is calculated as a function of radial position on the sun disk. The solar disk is divided by 11 concentric rings starting with an inner radius RI and an outer radius RO.…”
Section: Filling Factors Computationmentioning
confidence: 99%
“…The calculated filling factors for a feature reflect the fraction of the solar disk covered by the feature and assign reference synthetic spectra to it. [12] The filling factor is calculated as a function of radial position on the sun disk. The solar disk is divided by 11 concentric rings starting with an inner radius RI and an outer radius RO.…”
Section: Filling Factors Computationmentioning
confidence: 99%
“…The calculated filling factors for a feature reflect the fraction of the solar disk covered by the feature and the assignment of reference synthetic spectra to it has applications to modelling the Solar Spectral Irradiance [11]. The filling factor is calculated as a function of radial position on the sun disk.…”
Section: Filling Factors Computationmentioning
confidence: 99%
“…The fact that the TSI is on average higher near sunspot maximum implies that the influence of faculae and network is greater than that of sunspots (Fröhlich & Lean, 1998). Proxy-based models (see, Ashamari et al, 2015, for a recent review) try to answer the question: to what extent specific solar proxies, such as sunspot number, Mg II index, F10.7 radio flux, abundance of cosmogenic isotopes, spectral lines or specific wavelength bands in the observed solar spectra or solar intensitygrams, can be used to describe solar irradiance variability. This proxy-based empirical model is very successful in reproducing the observed TSI variations from 1978 to 2004, but it fails to explain the decrease observed since 2005 (Fröhlich, 2009).…”
Section: Introductionmentioning
confidence: 99%