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25 November 2014 Ozone vertical flux within the lower troposphere over background areas of west Siberia
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Proceedings Volume 9292, 20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics; 92925J (2014) https://doi.org/10.1117/12.2074519
Event: 20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, 2014, Novosibirsk, Russian Federation
Abstract
In this paper the results of the vertical ozone flux profiles calculated within the lower troposphere over background area of west Siberia are presented. The data on the vertical distribution of the ozone and meteorological parameters derived from AN-2 aircraft measurements supplemented by radiosonde launches. Profiles of turbulent diffusion coefficient were calculated based on “K-theory” with the use of nonlocal closure scheme – “Troen and Mahrt”. Calculations confirmed earlier findings that the formation of the daytime ozone maximum in the atmospheric boundary layer occurs due to its photochemical production from precursors.
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P. N. Antokhin, O. Yu. Antokhina, S. B. Belan, B. D. Belan, A. V. Kozlov, O. A. Krasnov, and D. A. Pestunov "Ozone vertical flux within the lower troposphere over background areas of west Siberia", Proc. SPIE 9292, 20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, 92925J (25 November 2014); https://doi.org/10.1117/12.2074519
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