The path of NLK whistler-mode signals received at Wellington

Details The path of NLK whistler-mode signals received at Wellington The path of NLK whistler-mode signals received at Wellington

May 1976

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1976p%26ss...24..443t&link_type=abstract

Planetary and Space Science, vol. 24, May 1976, p. 443-446. Research supported by the University Grants Committee.

Physics

Ionospheric Propagation, Propagation Modes, Signal Reception, Very Low Frequencies, Whistlers, Geomagnetic Latitude, Histograms, Magnetic Effects, Pulse Communication, Radio Attenuation, Time Lag

Scientific paper

VLF whistler-mode signals transmitted from NLK in Seattle, Wash., and received at Wellington, New Zealand, were found to travel mainly along magnetic-field lines near Wellington (L about 2.3) rather than those near Seattle (L about 3.0). This is found to be explicable in terms of the expected attenuation for the subionospheric part of the path together with the guiding to be expected from likely duct enhancements.

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