Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 27, Issue 1, Pages 53-56Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/1999GL003637
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From June 1994 to December 1995 the Ulysses spacecraft was within 3 AU of the Sun and traveled from high southern to high northern heliospheric latitudes. For this period, SWOOPS instrument data obtained when the magnetic field was approximately aligned with the radial direction from the Sun have been analyzed. In the fast wind at high latitudes, two resolvable proton components are typically present. Statistical studies of the relative densities and the field- aligned velocity difference, upsilon(omicron), of the two components are carried out, considering the dependence on distance from the Sun, the local Alfven speed, and the type of solar wind flow. The observed values of upsilon(omicron)/upsilon(A), where upsilon(A) is the local Alfven speed, are less than the upper bound determined from the linear theory for electromagnetic proton-proton instabilities. This result is good evidence that these microinstabilities constrain the relative streaming of the two components in the solar wind.
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