Table 2: From left to right: rms-velocity averaged over the convectively unstable region and time, correlation time from the autocorrelation of the vertical velocity, turnover time from test particle trajectories, and the Strouhal number. The last column states the number of snapshots with respect to which the correlation times and lengths were calculated.
Run $u_{\rm t}$ $\tau _{\rm c}$ $t_{\rm to}$ ${\rm St}$ N
lCo0 0.085 $11.2 \pm 2.3$ 25.9 0.43 209
Co0 0.084 $9.4 \pm 2.1$ 25.1 0.37 206
mCo0 0.080 $8.8 \pm 2.6$ 24.0 0.37 212
hCo0 0.073 $8.9 \pm 1.6$ 23.4 0.38 199
Co01-00 0.084 $9.4 \pm 2.2$ 25.0 0.38 206
Co01-30 0.084 $9.2 \pm 1.5$ 25.1 0.37 202
Co01-60 0.082 $9.8 \pm 2.9$ 25.0 0.39 207
Co01-90 0.082 $9.0 \pm 1.6$ 25.5 0.35 203
Co1-00 0.083 $7.3 \pm 1.4$ 24.5 0.30 207
Co1-30 0.086 $6.1 \pm 0.9$ 23.4 0.26 198
Co1-60 0.084 $6.9 \pm 0.8$ 23.7 0.29 207
Co1-90 0.083 $7.1 \pm 0.9$ 23.8 0.30 206
Co10-00 0.201 $2.2 \pm 0.3$ 12.6 0.17 202
Co10-30 0.072 $3.9 \pm 0.3$ 21.0 0.19 200
Co10-60 0.062 $3.4 \pm 0.2$ 20.5 0.17 201
Co10-90 0.062 $3.1 \pm 0.4$ 18.4 0.17 201


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