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Estimation of CO_2 Fluxes in the 'Atmosphere–Water' System in the South Lake Baikal Littoral with the Floating Chamber Method

机译:浮室法估算南贝加尔湖沿岸“大气-水”系统中的CO_2通量

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摘要

In this work, we discuss the applicability of the chamber method for measurements of carbon dioxide fluxes between the atmosphere and water in the littoral of Lake Baikal. Advantages and disadvantages of the method are considered. Previously submitted data are compared with observations in 2011–2014, when dramatically different weather situations occurred. It is shown that interannual variations in the total CO_2 fluxes are much weaker than their seasonal variations. The annual flux of carbon dioxide from atmo- sphere to the water surface in the littoral of Lake Baikal is assessed to be at least 6.5–7 g/m~2 per year in an "open water" period.
机译:在这项工作中,我们讨论了腔室法在测量贝加尔湖沿岸大气与水之间的二氧化碳通量时的适用性。考虑了该方法的优点和缺点。将之前提交的数据与2011-2014年的观测值进行比较,当时发生了截然不同的天气情况。结果表明,总CO_2通量的年际变化比其季节变化要弱得多。在“开放水域”期间,每年从大气到贝加尔湖沿岸的水面的二氧化碳通量估计为每年至少6.5–7 g / m〜2。

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