Abstract

RIOMETER investigations on auroral absorption events have been carried out so far by various experimenters in Alaska1, Canada2 and Scandinavia3. The characteristics of the auroral type of riometer absorption are normally given as follows: Auroral absorption is associated with the occurrence of visible aurora and magnetic disturbances. It is normally highly irregular in character, and although it may continue for a number of hours the individual peaks last only a few minutes.

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