Vol. 28, issue 06, article # 10

Abstract:

In this paper, we discuss the applicability of the chamber method for measuring the fluxes of carbon dioxide between the atmosphere and water in the littoral of Lake Baikal. Its advantages and disadvantages are considered as well. A comparison of previously submitted data with observations in 2011–2014, in which there were dramatically different weather situations, is presented. It is shown that interannual variations of total CO₂ fluxes is much less than its seasonal changes. It is shown that the annual flux of carbon dioxide from atmosphere to the water surface in littoral of Lake Baikal is at least 6.5–7 g per square meter in the "open water" period.

Keywords:

carbon dioxide flux, “atmosphere–water” system, chamber method, Lake Baikal, total flux

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