Vertical ozone flux in the near-surface layer of a background region of Western Siberia in 2016

P. N. Antokhin; O. Yu. Antokhina; B. D. Belan

doi:10.1117/12.2287121

30 November 2017 Vertical ozone flux in the near-surface layer of a background region of Western Siberia in 2016

P. N. Antokhin, O. Yu. Antokhina, B. D. Belan

Proceedings Volume 10466, 23rd International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics; 104665R (2017) https://doi.org/10.1117/12.2287121
Event: XXIII International Symposium, Atmospheric and Ocean Optics, Atmospheric Physics, 2017, Irkutsk, Russian Federation

Abstract

Vertical flux of ozone and the dry deposition rate have been calculated with the data measured at a high weather tower installed at the territory of Fonovaya (Background) Observatory of IAO SB RAS. The measurements were conducted in the period from February till July of 2016. It is shown that there are well pronounced diurnal dynamics of the vertical ozone flux and the dry deposition rate, which are inverse with respect to each other.

Citation Download Citation

P. N. Antokhin, O. Yu. Antokhina, and B. D. Belan "Vertical ozone flux in the near-surface layer of a background region of Western Siberia in 2016", Proc. SPIE 10466, 23rd International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, 104665R (30 November 2017); https://doi.org/10.1117/12.2287121

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