NON-STATIONARY TURBULENT REGIME IN THE SURFACE LAYER OF THE ATMOSPHERE.
AMERICAN METEOROLOGICAL SOCIETY BOSTON MASS
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Regularities in the vertical distribution of wind and temperature are ascertained for non-stationary conditions in a region of small values of dimensionless height. The problem of the quasi-stationary transformation of the temperature field is studied as a function of changes in the shortwave insolation. The relationships obtained can be used in forecasting. Author