Delayed storm-time increases in the whistler rate at mid-latitudes

Details Delayed storm-time increases in the whistler rate at mid-latitudes Delayed storm-time increases in the whistler rate at mid-latitudes

Nov 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975jatp...37.1423a&link_type=abstract

Journal of Atmospheric and Terrestrial Physics, vol. 37, Nov. 1975, p. 1423-1426.

Physics

Magnetic Storms, Midlatitude Atmosphere, Spread F, Whistlers, Correlation, Ionospheric Storms, Latitude, Magnetic Effects, Plasmapause, Signal Analysis, Time Dependence, Vlf Emission Recorders

Scientific paper

The occurrence of whistlers during 105 magnetic storms in the period between 1963 and 1968 is studied. Evidence that more whistlers occur during the storm recovery period is presented. Assuming that the increased whistler rate implies the presence of more ducts, similarities are noted between the storm-time duct population and the incidence of midlatitude spread-F in both time and space. It is suggested that a fresh examination of the physical processes involved in spread-F may aid the understanding of the formation of whistler ducts.

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