Abstract

Frequency spectra of atmospheric turbulenceSα(f) in the inertial subrange are considered in the free convection regime over the sea surface in a case of motionless instrument measurements (Eulerian frequency spectra). The frequency spectra formulaef*Sα(f)/σα2 =cα(f*/f)5/3 for wind velocity (α=1–3), temperature (α=t) and humidity (α=e) fluctuations are derived on the basis of similarity theory and the “−5/3 law”. These relations also can be derived from a consideration of convective large-scale advection of small eddies. The frequency scalef* = (N1β2/∈)1/2 ≈ (βH/z2)1/3 is the lower bound of the inertial subrange and it is of order 10−2 Hz.

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