The earth as a radio source

Abstract

Satellite measurements of the natural LF radio emission of the earth's magnetosphere are summarized, and the earth is compared as radio source to such familiar sources as Jupiter, Saturn and the sun. Two principal modes of radio emission from the earth's magnetosphere have been identified: auroral km-wavelength radiation and a continuum radiation. Characteristic spectra of the two modes are displayed. Other modes, not yet studied in much detail, are: dayside km-wavelength radiation, emission upstream of the bow shock, and narrow-bandwidth radio bursts. Emissions from the Jovian moon Io and from pulsars are also drawn upon for comparison. Current views on the sources of these terrestrial radio emissions are summarized.