Abstract
We considered the results of the complex measurements of meteorological parameters at two observation sites in Moscow with the help of Volna-4 sodar, the Meteo-2 ultrasonic meteorological station, and the MTP-5 meteorological temperature profiler. The frequency of occurrence and the heights of temperature inversion boundaries under the conditions of woodland-park zone are analyzed. The obtained results are compared with analogous estimates of some other authors for the central part of the city. It is found that a stable stratification of the urban roughness sublayer takes place considerably more often in the woodland-park zone of the city than in the central part of the urbanized territory.
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