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An example of anticorrelation of auroral particles and electric fields.The question of whether correlation or anticorrelation should occur is complex and depends on many factors, e.g., the internal impedance of the source; the Pedersen conductivity, which in turn is dependent on the incident energy of the precipitated particles; whether space charge can build up; and the magnitude of the incoming flux. Data are presented from a case in which an anticorrelation between auroral particles and electric fields is especially striking. The data were obtained from a Nike Tomahawk launched from the Norwegian rocket range at Andoya. The experiments carried are described briefly. The data support the anticorrelation model as one mechanism that can affect the electric field strength in auroral regions.
Document ID
19730051495
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Maynard, N. C.
(NASA Goddard Space Flight Center Greenbelt, Md., United States)
Bahnsen, A.
(Danish Space Research Institute Lyngby, Denmark)
Christophersen, P.
Lundin, R.
(Kiruna Geofysiska Observatorium Kiruna, Sweden)
Egeland, A.
(Norske Institutt for Kosmisk Fysikk Oslo, Norway)
Date Acquired
August 7, 2013
Publication Date
July 1, 1973
Publication Information
Publication: Journal of Geophysical Research
Volume: 78
Subject Category
Geophysics
Accession Number
73A36297
Distribution Limits
Public
Copyright
Other

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