Abstract
The Obukhov-Kolmogorov (OK) theory has provided us with the very well- known –11/3-power spectrum; widely assumed as a valid model for the refractive index fluctuations in the whole atmosphere. Within its reach, the strength of the fluctuations are conveyed by the structure constant, . Yet, the OK model presupposes the existence of statistical isotropy and homogeneity–both for the velocity and refractive index fluctuations. In this work, we show that this is a rare occurrence in turbulent airflow above the ocean. Therefore, we need to re-evaluate the physical meaning of measurements.
© 2021 The Author(s)
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