Abstract Electron density profiles measured by the EISCAT incoherent scatter radar are used to derive the Hall- and Pedersen conductances and the characteristic energy of the incoming particles during events of strong particle precipitation. A relationship is sought between the Hall- to Pedersen conductance ratio, R, and the root mean square energy, Erms, which can be expressed by: E rms = A exp( R B ) where A and B are constants to be determined in the text.


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    Title :

    EISCAT studies of the auroral ionosphere conductances


    Contributors:
    Brekke, A. (author) / Hall, C. (author) / Hansen, T.L. (author)

    Published in:

    Publication date :

    1989-01-01


    Size :

    4 pages




    Type of media :

    Article (Journal)


    Type of material :

    Electronic Resource


    Language :

    English




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