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Effect of possible passage through Halley's magnetic tail on geomagnetic activityIt is found that there occurred a geomagnetic storm on May 18/19, 1910 that cannot be dismissed as a recurrent storm. The period of storminess is close to the period of time at which the magnetic and plasma tail of Halley should have passed over the earth. The signature is worldwide and of the form and magnitude expected if the solar wind were shielded from the earth by the comet. Comparison with computer simulations applicable closer to the comet suggests that this interpretation is feasible. If this interpretation is correct, the 'lobes' of the Halley tail have deeper lows at 24 x 10 to the 6th km than in the present model at 7 x 10 to the 6th km downstream and are at least twice as wide.
Document ID
19880026266
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Russell, C. T.
(California Univ. Los Angeles, CA, United States)
Phillips, J. L.
(California, University Los Angeles, United States)
Fedder, J. A.
(U.S. Navy, Naval Research Laboratory, Washington DC, United States)
Allen, J. H.
(California Univ. Los Angeles, CA, United States)
Morris, L.
(NOAA, National Geophysical Data Center Boulder, CO, United States)
Craig, Roger A.
(NASA Ames Research Center Moffett Field, CA, United States)
Date Acquired
August 13, 2013
Publication Date
October 1, 1987
Publication Information
Publication: Journal of Geophysical Research
Volume: 92
ISSN: 0148-0227
Subject Category
Geophysics
Report/Patent Number
ISSN: 0148-0227
Accession Number
88A13493
Funding Number(s)
CONTRACT_GRANT: NAGW-717
Distribution Limits
Public
Copyright
Other

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