2005
DOI: 10.1615/telecomradeng.v64.i10.100
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Two Component Model of the Schumann Resonance Signal

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Cited by 6 publications
(7 citation statements)
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“…A substantial part of global lightning activity is omitted by OTD and hence is absent in the model simulations. This activity is present as the “background” in the SR records (the characteristics of the background were studied by Yatsevich et al [2005]) and hence the minimum‐maximum difference in the experimental records is significantly smaller then the minimum‐maximum difference in the model simulations that base on OTD data (this was also noted by Hayakawa and Nickolaenko [2005] and Nickolaenko et al [2006]).…”
Section: Simulations With Global Lightning Distributionmentioning
confidence: 87%
“…A substantial part of global lightning activity is omitted by OTD and hence is absent in the model simulations. This activity is present as the “background” in the SR records (the characteristics of the background were studied by Yatsevich et al [2005]) and hence the minimum‐maximum difference in the experimental records is significantly smaller then the minimum‐maximum difference in the model simulations that base on OTD data (this was also noted by Hayakawa and Nickolaenko [2005] and Nickolaenko et al [2006]).…”
Section: Simulations With Global Lightning Distributionmentioning
confidence: 87%
“…SR are mainly excited by the cloud‐to‐ground lighting discharges in the atmosphere, and carry information about the global lightning activity in three main thunderstorm regions (Africa, southeast Asia, and South America) and electromagnetic properties of the lower ionosphere. The long‐term SR records collected at several different stations have been reported in many papers [e.g., Sátori et al , 1996; Nickolaenko et al , 1998; Price and Melnikov , 2004; Yatsevich et al , 2006; Sekiguchi et al , 2008]. The clear diurnal and seasonal variations of SR power and frequency were observed.…”
Section: Introductionmentioning
confidence: 99%
“…Two source models are used. The first, the simple model is the compact source [Yatsevich et al, 2006[Yatsevich et al, , 2008: the global thunderstorms occupy a compact area (15°radius) at the equator and move around the globe during the day. The source intensity appropriately varies in time.…”
Section: Appendix Amentioning
confidence: 99%
“…Pronounced seasonal/diurnal variations in Figure 1 occur at a “podium” present in records of all three observatories, i.e., the diurnal curve is elevated over the abscissa and never reaches the zero level. This vertical shift regarded as “podium,” originates from the “inappropriate” thunderstorm activity distributed over the whole globe and causing the depolarized SR signals at an observatory [ Yatsevich et al , 2006, 2008].…”
Section: Separating the Lt And Ut Componentsmentioning
confidence: 99%