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Analysis of phase coherence in fully developed atmospheric turbulence: Amazon forest canopy

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Figure

Fig. 1. Time series of temperatureabove the Amazon forest canopy (left panels) and within the Ama-zon canopy (right panels), taken from noon to 12:30 on Julian Day T and vertical wind velocity w068, 1999.
Fig. 2. Scale dependence of the normalized temperature-difference�T and the normalized vertical wind velocity-difference �w abovethe Amazon forest canopy for three different time scales (τ=0.15 s,3.3 s and 100 s).
Fig. 5. Probability density distribution (PDF) of the normalizedvertical wind velocity-difference �w (left panels) and the normal-ized temperature-difference �T (right panels) fluctuations withinthe Amazon forest canopy for three different time scales (τ=0.15 s,3.3 s and 100.0 s), superposed by a Gaussian PDF (gray line).
Fig. 6. Kurtosis and Phase Coherence Index of vertical wind veloc-ities (left panels) and temperatures (right panels) above and withinthe Amazon forest canopy

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