  Turbulent convection systems are known to give rise to prominent large scale
circulation. At the same time, the `background' (or `small-scale') turbulence
is also highly relevant and e.g. carries the majority of the heat transport in
the bulk of the flow. Here, we investigate how the small-scale turbulence is
interlinked with the large-scale flow organization of Rayleigh-B\'enard
convection. Our results are based on a numerical simulation at Rayleigh number
$Ra = 10^8$ in a large aspect ratio ($\Gamma=32$) cell to ensure a distinct
scale separation. We extract local magnitudes and wavenumbers of small scale
turbulence and find significant correlation of large scale variations in these
quantities with the large-scale signal. Most notably, we find stronger
temperature fluctuations and increased small scale transport (on the order of
$10\%$ of the global Nusselt number $Nu$) in plume impacting regions and
opposite trends in the plume emitting counterparts. This concerns wall
distances up to $2\delta_\theta$ (thermal boundary layer thickness). Local
wavenumbers are generally found to be higher on the plume emitting side
compared to the impacting one. A second independent approach by means of
conditional averages confirmed these findings and yields additional insight
into the large-scale variation of small-scale properties. Our results have
implications for modelling small-scale turbulence.
