Measurements of the intensities of the O VI 1032 and 1037 Angstrom spectral
lines in the southern solar hemisphere, from 1.5 to 5 R-s, were made with
the SOHO Ultraviolet Coronagraph Spectrometer (UVCS) in May 2000 close to s
olar maximum. The ratio of the intensity of the two oxygen lines is used as
a proxy for solar wind velocity in the inner corona. White light images of
the corona taken with the SOHO/LASCO-C2 during the same time period, and u
sed to place the UVCS observations in the context of coronal structures, sh
ow streamers extending to high latitudes. The measured radial and azimuthal
gradients of the intensity ratio reflect strong velocity shears in the cor
ona with the slowest wind coinciding with the axis of streamers. Comparison
of these results with ratios measured with UVCS during solar minimum indic
ates that the transition from fast to slow wind in the inner corona occurs
within 20 degrees of the axis of streamers at both phases of the solar cycl
e.