Using polarized brightness (pB) measurements made by the High Altitude Obse
rvatory (HAO) Mauna Loa Mk III K-coronameter, we investigate the daily chan
ges of path-integrated density at 1.15 R-circle dot. During 1996, when simu
ltaneous pB and helioseismology data were available, we find that the corre
lation of pB (at zero time lag and 20 degrees latitude lag) varies with lat
itude in the same way that the subsurface differential rotation inferred fr
om helioseismology does. The association is such that bands of higher pB co
rrelation are associated with retrograde subsurface rotation and that lower
pB correlation bands are associated with prograde subsurface rotation. We
also show that polar coronal holes are distinguished by a nonrecurring long
itudinal structure as opposed to a recurring structure in the quiet Sun. In
addition, the levels of pB and standard deviation sigma(pB) of pB are abou
t half of those of the neighboring quiet Sun. These statistical characteris
tics of coronal density in polar holes and the quiet Sun were also present
in 1993-1994 and are replicated in the statistics of the distant solar wind
observed by Ulysses. The association of the density (pB) correlation with
subsurface flow (when simultaneous data were available in 1996), together w
ith the association of the latitudinal dependence of the statistical charac
teristics (average, standard deviation, and autocorrelation function) of th
e coronal (pB) and solar wind (Ulysses) density (when simultaneous data wer
e available in 1993-1994), suggest a correlated variability of subsurface f
low, coronal density, and solar wind density organized by solar latitude.