The vertical velocity variance during convective activity was measured with an acoustic Doppler sounder. Here we show that this technique provides measurement of the heat flux profile in the well-mixed surface layer and gives a reference height h prime related to the inversion height Z//I during the mornings. It is shown that the structure function of temperature fluctuations C//T**2 can be obtained by these measurements using the A. M. Kaimal et al.
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Weill, A., Klapisz, C., Strauss, B., Baudin, F., Jaupart, C., Van Grunderbeeck, P., & Goutorbe, J. P. (1980). MEASURING HEAT FLUX AND STRUCTURE FUNCTIONS OF TEMPERATURE FLUCTUATIONS WITH AN ACOUSTIC DOPPLER SODAR. Journal of Applied Meteorology, 19(2), 199–205. https://doi.org/10.1175/1520-0450(1980)019<0199:MHFASF>2.0.CO;2