Estimation of contributions from different-scale components of the wind vector and air temperature to turbulent heat fluxes in the atmospheric surface layer

Fluxes of air temperature in the atmospheric surface layer have been calculated from experimental data obtained with the ultrasonic anemometer-thermometer. Estimates of temperature fluxes of the “turbulent” and “local” scales along three axes of the Cartesian coordinate system in the summer period over an urban territory have been considered. The fluxes observed in the day and night time have been compared.

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