We used the time correlation of shadowgraph images to determine the angle
Θ of the horizontal component of the plume velocity above (below) the
center of the bottom (top) plate of a cylindrical Rayleigh-B\'enard cell of
aspect ratio Γ≡D/L=1 (D is the diameter and L≃87 mm
the height) in the Rayleigh-number range 7×107≤R≤3×109 for a Prandtl number σ=6. We expect that Θ gives the
direction of the large-scale circulation. It oscillates time-periodically. Near
the top and bottom plates Θ(t) has the same frequency but is
anti-correlated.Comment: 4 pages, 6 figure