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Temperature time traces are obtained in turbulent thermal convection at highRayleigh numbers. Measurements are made in the midplane of the apparatus, nearthe sidewall but outside the boundary layer. A telegraph approximation fortemperature traces is generated by setting the fluctuation amplitude to 1 or 0depending on whether or not it exceeds the mean value. Unlike the standarddiagnostics of intermittency, the telegraph approximation allows one todistinguish the tendency of events to cluster ("clusterization") from theirlarge-scale variability in amplitude. A qualitative conclusion is thatamplitude intermittency might mitigate clusterization effects

“Clusterization” and intermittency of temperature fluctuations in turbulent convection