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Effect of Global Warming on the Stratospheric Ozone Depletion Rate in Catalytic Cycles

  • CHEMICAL PHYSICS OF ATMOSPHERIC PHENOMENA
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Abstract

Data on the change in the rate of stratospheric ozone depletion in the Ox, HOx, NOx, ClOx, and BrOx catalytic cycles as a result of a change in the stratospheric temperature caused by global warming in 2100 compared with 2000 were presented. The altitude profiles of the concentrations of minor atmospheric components and temperature were calculated using the SOCRATES interactive two-dimensional model for the conditions of June and January 2000 and 2100 at a latitude of 50° N and altitudes in the range 0–50 km. The forecasts on the atmospheric contents of greenhouse gases of the Intergovernmental Panel on Climate Change RCP 4.5 and RCP6.0 for 2000 and 2100 were used as initial data for calculations.

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Notes

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Funding

This study was financially supported by the Russian Foundation for Basic Research (grant no. 19-05-00080).

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Authors and Affiliations

  1. Talrose Institute of Energy Problems of Chemical Physics, Semenov Federal Research Center of Chemical Physics, Russian Academy of Sciences, 119991, Moscow, Russia

    I. K. Larin

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  1. I. K. Larin
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Correspondence to I. K. Larin.

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Translated by L. Smolina

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Larin, I.K. Effect of Global Warming on the Stratospheric Ozone Depletion Rate in Catalytic Cycles. Russ. J. Phys. Chem. B 14, 344–350 (2020). https://doi.org/10.1134/S1990793120020256

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