Daily Course of CO2 Fluxes in the Atmosphere–Water System and Variable Fluorescence of Phytoplankton during the Open-Water Period for Lake Baikal according to Long-Term Measurements


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Аннотация

The process of gas exchange of CO2 in the atmosphere–water system and its relation to the daily course of variable fluorescence of phytoplankton is studied on the basis of long-term (2004–2014) measurements during the open water period for Lake Baikal. It is found that the decrease in photosynthetic activity of plankton is almost synchronous to the increase in the CO2 flux from atmosphere to water. It follows from comparison of the spring and summer data with December measurements that the daily decrease in variable fluorescence of phytoplankton is caused by the internal daily rhythm of the photosynthetic activity of plankton.

Авторлар туралы

V. Zavoruev

Siberian Federal University; Institute of Computational Modeling, Siberian Branch

Хат алмасуға жауапты Автор.
Email: valzav@icm.krasn.ru
Ресей, Krasnoyarsk, 660041; Krasnoyarsk, 660036

V. Domysheva

Institute of Computational Modeling, Siberian Branch

Email: valzav@icm.krasn.ru
Ресей, Krasnoyarsk, 660036

D. Pestunov

Zuev Institute of Atmospheric Optics, Siberian Branch

Email: valzav@icm.krasn.ru
Ресей, Tomsk, 634055

M. Sakirko

Limnological Institute, Siberian Branch

Email: valzav@icm.krasn.ru
Ресей, Irkutsk, 664033

M. Panchenko

Zuev Institute of Atmospheric Optics, Siberian Branch

Email: valzav@icm.krasn.ru
Ресей, Tomsk, 634055

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