Происхождение ночных максимумов фоновых концентраций приземного озона в юго-восточном крыму
DOI:
https://doi.org/10.15587/2313-8416.2015.49327Słowa kluczowe:
концентрация приземного озона, суточный ход приземного озона, ночные максимумы, миграцияAbstrakt
Работа посвящена исследованию причин и факторов появления ночных максимумов концентрации приземного озона, наблюдающихся при его измерениях на станции Фонового экологического мониторинга Карадагского природного заповедника. Показано, что вероятной причиной повышения в ночные часы фоновых концентраций озона является увеличение средних скоростей ветра в приземном слое атмосферы. Это приводит к усилению турбулентной диффузии, что активизирует вертикальную миграцию воздуха
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