Abstract
Analysis of the mechanisms determining the direction and intensity of CO2 fluxes in the “atmosphere-water” system seems to be important in the context of studying the problem of present-day increase in the content of one of the greenhouse gases (carbon dioxide) in the atmosphere. This paper starts a series of publications devoted to the analysis of seasonal features of the CO2 gas exchange process in the littoral zone of southern Baikal and presents the results obtained in the spring period.
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