Data on the relative contribution of the Ox, HOx, NOx, ClOx, BrOx, and IOx catalytic cycles to atmospheric ozone destruction are given for June and January 2000 at a latitude of 50° N in the height range of 0–50 km. The height profiles of the components of the above families have been calculated using the SOCRATES two-dimensional interactive model and the one-dimensional photochemical model developed at the Tal’rose Institute of Energy Problems of Chemical Physics, Russian Academy of Sciences. The initial data for the calculations are taken to be the atmospheric content of greenhouse gases according to the Intergovernmental Panel on Climate Change RCP 4.5 scenario for 2000. The ozone destruction rate is calculated using an algorithm proposed earlier by the author to determine the rate of the limiting stage of the catalytic cycle.

中文翻译：

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在 Ox、HOx、NOx、ClOx、BrOx 和 IOx 催化循环中破坏大气臭氧

提供了 2000 年 6 月和 2000 年 1 月在北纬 50°、高度范围 0-50 公里处的 Ox、HOx、NOx、ClOx、BrOx 和 IOx 催化循环对大气臭氧破坏的相对贡献的数据。上述各族组件的高度分布是使用俄罗斯科学院塔尔罗斯化学物理能源问题研究所开发的 SOCRATES 二维交互模型和一维光化学模型计算得到的。根据政府间气候变化专门委员会 2000 年的 RCP 4.5 情景，计算的初始数据是温室气体的大气含量。臭氧破坏率是使用作者早先提出的算法计算的，以确定臭氧破坏率。催化循环的极限阶段。