2008
DOI: 10.1134/s0010952508040011
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Reconstruction of space weather physical parameters on 400-year scale

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Cited by 9 publications
(3 citation statements)
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“…Figure 5 shows a comparison made by Mun ˜oz-Jaramillo et al (2015) of fits to the instantaneous total group sunspot number area from RGO for four different functions: lognormal, power law, exponential, and Weibull. For the five data sets Mun ˜oz-Jaramillo et al considered (RGO, KMAS, SOON, Pulkovo Observatory (Nagovitsyn et al 2008), and the Heliospheric and Magnetic Imager (HMI; Scherrer et al 2012) on the Solar Dynamics Observatory (SDO; Pesnell et al 2012), the best fit was provided by the Weibull function distribution in each case although it only passed the Kolomogorov-Smirnov test for the HMI data set.…”
Section: Related Workmentioning
confidence: 99%
“…Figure 5 shows a comparison made by Mun ˜oz-Jaramillo et al (2015) of fits to the instantaneous total group sunspot number area from RGO for four different functions: lognormal, power law, exponential, and Weibull. For the five data sets Mun ˜oz-Jaramillo et al considered (RGO, KMAS, SOON, Pulkovo Observatory (Nagovitsyn et al 2008), and the Heliospheric and Magnetic Imager (HMI; Scherrer et al 2012) on the Solar Dynamics Observatory (SDO; Pesnell et al 2012), the best fit was provided by the Weibull function distribution in each case although it only passed the Kolomogorov-Smirnov test for the HMI data set.…”
Section: Related Workmentioning
confidence: 99%
“…The result is a set of 19038 groups. PCSA data is available at http://www.gao.spb.ru/database/csa/, and is described in detail by Nagovitsyn et al (2008). Data are shown in Figure 1(b).…”
Section: Sunspot Group Databasesmentioning
confidence: 99%
“…An approach involving "time scales," which are dis tinguished in accordance with our possibilities for using observational material for reconstructions, was proposed in (Nagovitsyn et al, 2004(Nagovitsyn et al, , 2008. We distinguish the fol lowing successive scales: (a) 100-150 years, direct regu lar solar activity observations; (b) 400 years, irregular direct activity observations; (c) 1000-2000 years, the selection of indirect data on solar activity (auroras and sunspots observed by naked eye and radionuclides in nat ural archives); (d) 10000 years, indirect data (called "proxies" in English literature) on solar activity: data on the radiocarbon and beryllium 10 concentration in dated samples (tree rings, polar ice); (e) more than 10000 years, hypothetical data (thickness of varve and clay laminas), the origin of which is related to solar activity according to some researchers.…”
Section: Introductionmentioning
confidence: 99%