Техника и методика геофизического эксперимента : сборник научных трудов / Рос. акад. наук, Кол. науч. центр, Поляр. геофиз. ин-т. – Апатиты : [б. и.], 2003. – 194 с.

Using the dynamical model o f the atmosphere surface layer, as the basis, the paper suggests a hypothesis on the similarity o f the ozone vertical profile and basic meteorological parameters. Basing on the above said, we offer a solution to the problem o f restoration o f the ozone profile only bay 2 values o f its concentration, using more easily accessible results o f wind velocity measurements at various levels. It is also suggested, that the discrepancy between the actual profile and the aestivated one would enable us to judge about the existence o f mechanisms o f its photochemical destruction and generation in the surface layer. An estimation o f the ozone destruction rate on the snow-covered surface has been carried out by the results of an experiment, according to the adopted model. Ref. - 7 titles. 194