We have studied an outstanding sequence of continuum images of the sol
ar granulation from Pic du Midi Observatory. We have calculated the ho
rizontal vector flow field using a correlation tracking algorithm, and
from this determined three scalar fields: the vertical component of t
he curl, the horizontal divergence, and the horizontal flow speed. The
divergence field has substantially longer coherence time and more pow
er than does the curl field. Statistically, curl is better correlated
with regions of negative divergence-that is, the vertical vorticity is
higher in downflow regions, suggesting excess vorticity in intergranu
lar lanes. The average value of the divergence is largest (i.e., outfl
ow is largest) where the horizontal speed is large; we associate these
regions with exploding granules. A numerical simulation of general co
nvection also shows similar statistical differences between curl and d
ivergence. Some individual small bright points in the granulation patt
ern show large local vorticities.