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By results of carrying out of several series of direct atmospheric air pumping the data which allow to draw a conclusion that contents in atmospheric air are in dependence from a season and weather conditions are obtained. In rains and downpours of the mercury contents in atmospheric air aspire to zero (since there is a washing away of mercury from atmosphere), and during the solar periods they a little above and reach several tens ng/m3 that also is connected with activization of mercury emission from soils. Monitoring supervision have shown that variations are significant enough and change from day by day. Difference consists only that in the areas removed from obvious sources of pollution, fluctuations occur in small limits.