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Equatorial irregularity belt and its movement during a magnetic stormEvidence for an equatorial irregularity belt and its movement during a magnetic storm has been obtained from Faraday rotation measurements at a chain of 140-MHz radio beacons receiving from the ATS-6 satellite. The stations covered a latitude region from the magnetic equator to the 45 deg N dip on the Indian subcontinent. An irregularity belt extending from the magnetic equator to about 27 deg N latitude was observed during the main phase of the magnetic storm of 10 January, 1976.
Document ID
19780047491
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
External Source(s)
doi:10.1038/272345a0
Authors
Vats, H. O. (Physical Research Lab. Ahmedabad, India)
Chandra, H. (Physical Research Lab. Ahmedabad, India)
Deshpande, M. R. (Physical Research Lab. Ahmedabad, India)
Rastogi, R. G. (Physical Research Laboratory Ahmedabad, India)
Murthy, B. S. (Indian Institute of Astrophysics Kodaikanal, India)
Janve, A. V. (Physical Research Lab. Ahmedabad, India)
Rai, R. K. (Udaipur, University Udaipur, India)
Singh, M. (Physical Research Lab. Ahmedabad, India)
Gurm, H. S. (Punjabi University Patiala, India)
Jain, A. R. (Indian Institute of Geomagnetism Bombay, India)
Date Acquired
August 9, 2013
Publication Date
March 23, 1978
Publication Information
Publication: Nature
Volume: 272
Subject Category
Geophysics
Accession Number
78A31400
Distribution Limits
Public
Copyright
Other

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