From June 1994 to December 1995 the Ulysses spacecraft was within 3 AU of t
he Sun and traveled from high southern to high northern heliospheric latitu
des. For this period, SWOOPS instrument data obtained when the magnetic fie
ld was approximately aligned with the radial direction from the Sun have be
en analyzed. In the fast wind at high latitudes, two resolvable proton comp
onents are typically present. Statistical studies of the relative densities
and the field- aligned velocity difference, upsilon(omicron), of the two c
omponents 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 c
omponents in the solar wind.