Excitation of the earth-ionosphere waveguide by downgoing whistlers. III - Wave normal not in the magnetic meridian

Details Excitation of the earth-ionosphere waveguide by downgoing whistlers. III - Wave normal not in the magnetic meridian Excitation of the earth-ionosphere waveguide by downgoing whistlers. III - Wave normal not in the magnetic meridian

Dec 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975jatp...37.1599w&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 37, Dec. 1975, p. 1599, 1600. Research supported by the South African Counc

Physics

Geomagnetic Latitude, Ionospheric Propagation, Waveguides, Whistlers, Atmospheric Attenuation, Goniometers, Phase Velocity

Scientific paper

Calculations relating to the excitation of the earth-ionosphere waveguide by downgoing whistlers carried out in previous papers are generalized to the case where the plane of incidence is not in the magnetic meridian. It is found that the results are very insensitive to the orientation of the plane of incidence. Thus previous results applying in the magnetic meridian plane can be applied to stations widely separated in longitude. In particular stations spaced in longitude by up to 2000 km should be able to receive the same whistlers.

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