Роль изменений солнечной активности и состояния озоносферы в глобальном затемнении земной атмосферы

Авторы

  • Александр Вадимович Холопцев Севастопольская морская академия ул. Рыбаков 7-а, г. Севастополь, 99055,
  • Мария Павловна Никифорова Севастопольский национальный технический университет ул. Университетская, 33, Севастополь, 99033,

DOI:

https://doi.org/10.15587/2313-8416.2014.29735

Ключевые слова:

глобальное затемнение, оптическая плотность облачности, солнечная активность, общее содержание озона

Аннотация

Выявлены расположения сегментов земной атмосферы, в которых значимыми факторами межгодовых вариаций среднемесячных значений оптической плотности  облачности, являются совпадающие с ними по времени изменения соответствующих значений общего содержания озона и чисел Вольфа. При дальнейшем увеличении содержания в атмосфере парниковых газов, влияние этих изменений на эффект  «глобального затемнения»  будет усиливаться.

Биографии авторов

Александр Вадимович Холопцев, Севастопольская морская академия ул. Рыбаков 7-а, г. Севастополь, 99055

Профессор, доктор географических наук, действительный член Крымской академии наук и академии наук Польши (комиссия по метеорологии и агроклиматологии)

Кафедра Судовождения и безопасности мореплавания

Мария Павловна Никифорова, Севастопольский национальный технический университет ул. Университетская, 33, Севастополь, 99033

Младший научный сотрудник

Кафедра физики

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Опубликован

2014-12-25

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Раздел

Географические науки