On the directional dependency of [`]slow tail' extremely low-frequency atmospheric waveforms

Details On the directional dependency of [`]slow tail' extremely low-frequency atmospheric waveforms On the directional dependency of [`]slow tail' extremely low-frequency atmospheric waveforms

May 1967

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1967jatp...29..545h&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 29, no. 5, pp. 545-550, IN3-IN5, 551-552

Physics

Scientific paper

Experimental evidence is presented that the [`]slow tail' atmospheric waveforms reported by Liebermann (1956) and Tepley (1959) which are classified as Type A and Type B are predominately easterly and westerly propagating waveforms, respectively. The effects of variations in the types of sources as a cause of the different types of waveforms are minimized by the comparison of [`]slow tail' waveforms generated by intracloud and cloud-to-ground type lightning discharges.

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