1970
DOI: 10.21236/ad0706873
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Research on Extremely Low Frequency Propagation With Particular Emphasis on Schumann Resonance and Related Phenomena. Part Ii. Location of Sources

Abstract: Administrative Information, • iii Table of Contents v Lint of Figures. , ix list of Symbols xii IV Cavity Fields From Vertical Electric Dipole Sources. 27 ^.1 The Earth-Ionosphere Cavity Model 27 4.2 Cavity Fields from Vertical Electric Dipole Sources 28 4.3 Fields from a Distribution of Independent Sources 31 Show more

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1971
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“…In the domain of the Schumann frequencies the possibility of monitoring the global lightning activh gained some momentum during the reporting period Polk [1969], , and Hughes {\9m discussed this item during the Tokyo conference Sir* then, especially during the March 7, 1970, solar eciip* new insight into frequency splitting has been obtained Also, it could be verified from ELF measurements tha> the contribution of the oceanic (Pacific) thunderstorm* occur mainly around local midnight, whereas other sources peak in the late local afternoon [Galejs, I9?f)i The cooperation of an ELF station near Kingston Rhode Island, with a station in southern German) continues. Location of thunderstorm centers with ex tremely low frequency, large changes in signal level m connection with solar proton events, the occurrence of ELF whistlers, and an indication of separation of the different influences by considering the power and resonant frequencies independently have been reported [Keefe and Polk, 1970], Toomey and Polk [1970],Polk [1969],and Keefe etal. [1968.…”
Section: Electromagnetic Radiation From Lightningmentioning
confidence: 99%
“…In the domain of the Schumann frequencies the possibility of monitoring the global lightning activh gained some momentum during the reporting period Polk [1969], , and Hughes {\9m discussed this item during the Tokyo conference Sir* then, especially during the March 7, 1970, solar eciip* new insight into frequency splitting has been obtained Also, it could be verified from ELF measurements tha> the contribution of the oceanic (Pacific) thunderstorm* occur mainly around local midnight, whereas other sources peak in the late local afternoon [Galejs, I9?f)i The cooperation of an ELF station near Kingston Rhode Island, with a station in southern German) continues. Location of thunderstorm centers with ex tremely low frequency, large changes in signal level m connection with solar proton events, the occurrence of ELF whistlers, and an indication of separation of the different influences by considering the power and resonant frequencies independently have been reported [Keefe and Polk, 1970], Toomey and Polk [1970],Polk [1969],and Keefe etal. [1968.…”
Section: Electromagnetic Radiation From Lightningmentioning
confidence: 99%