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Evidence of a large-scale gradient in the solar wind velocityMeasurements of the solar wind velocity are compared at two widely separated locations, using plasma data obtained by Mariner 5, en route to Venus, and with the near-earth satellites Explorer 33, 34, and 35. A previous study of the propagation of interplanetary sector boundaries between Mariner and the earth had implied the existence of large scale velocity gradient which was interpreted as a latitude gradient of approximately 13 km/sec per degree of latitude. The results of the present investigation in which the earlier results were extended to the overall solar wind, without regard to the presence of sector boundaries, suggests that a latitude dependence of the solar wind velocity is the most plausible interpretation of the large-scale velocity gradient.
Document ID
19760050075
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Rhodes, E. J., Jr.
(California Institute of Technology, Jet Propulsion Laboratory, Pasadena, Calif.; California, University Los Angeles, Calif., United States)
Smith, E. J.
(California Institute of Technology, Jet Propulsion Laboratory, Pasadena Calif., United States)
Date Acquired
August 8, 2013
Publication Date
May 1, 1976
Publication Information
Publication: Journal of Geophysical Research
Volume: 81
Subject Category
Solar Physics
Accession Number
76A33041
Funding Number(s)
CONTRACT_GRANT: NAS7-100
Distribution Limits
Public
Copyright
Other

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