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© Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. A method of gradient measurements regarding the concentration of ozone (O3) and atmospheric dynamic characteristics with the help of meteorological masts was used to study the effect of the thermal stratification of the atmosphere on ozone, and to study the characteristics of the exchange processes of trace gases (fluxes and rates of dry deposition) between the atmosphere and the underlying surface (grasslands, forest). The sample site is located within the territory of the Boyarsky stationary site (51◦830 N, 106◦060 E) of Institute of Physical Materials Science Siberian Branch, Russian Academy of Sciences, which is situated at a distance of 500 m from the Baikal water area, at heights of 60 m from the lake level. Air samples were taken at different heights above ground level using Teflon tubes. Observations were performed using chemiluminescent gas analyzers 3-02 P-A for ozone (OPTEK Corp., St. Petersburg, Russia). Simultaneously, the meteorological and turbulent parameters of the atmosphere were measured using the acoustic meteorological complexes: AMK-03 and EXMETEO (Sibanalitpribor Ltd., Tomsk, Russia). Atmosphere Experiments—Grasslands. To estimate the flux of ozone to the underlying surfaces, the calculations were conducted with proven methods (Erisman et al., 1994; Jacobson, 1999; Qin et al., 2004). To evaluate the flux of ozone to the underlying surfaces as a quantitative characteristic, the velocity and deposition rate of ozone are used (Equation (1)): F = −Vd × C (1)

Results of a comparative study of dry ozone deposition fluxes on grasslands and forest vegetation near Lake Baikal