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Юг России: экология, развитие

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Солнечная радиация 2600 BP и Малый ледниковый период как причины наслоений Каспийского моря

https://doi.org/10.18470/1992-1098-2008-4-15-25

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Аннотация

Исследования, включающие в себя социальное, экономическое и экологическое содержание, выявляют общность сопутствующих областей и глобальной цели. Эта цель скрыта за понятием "устойчивое развитие". Эти ограничения представлены как мультипликативный индекс развития. Этот индекс отражает информационный баланс определенной территории. Уровень Каспийского моря, наибольшего внутреннего моря в мире, сильно колебался в течение своей истории, с амплитудами до 3 м в прошлом столетии, до 25 м в последнем тысячелетии, и до более150 м начиная с Последнего Ледникового периода. Результаты показывают, что последние главные наслоения произошли приблизительно в 2600 г. до н.э. и в Малом Ледниковом периоде и совпадает с глобальным охлаждением, связанным с минимумами в солнечной активности. Это позволяет предположить, что тысячелетние изменения осадков в волжском речном бассейне также вызваны солнечной активностью.

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Для цитирования:


Крооненберг С.Б., Абдурахманов Г.М., Бадюкова Е.Н., Ван дер Борг К., Калашников А., Касимов Н.С., Рычагов Г.И., Свиточ А.А., Вонхов Х.Б., Весселинг Ф.П. Солнечная радиация 2600 BP и Малый ледниковый период как причины наслоений Каспийского моря. Юг России: экология, развитие. 2008;3(4):15-25. https://doi.org/10.18470/1992-1098-2008-4-15-25

For citation:


Kroonenberg S.B., Abdurakhmanov G.M., Badyukova E.N., van der Borg K., Kalashnikov A., Kasimov N.S., Rychagov G.I., Svitoch A.A., Vonhof H.B., Wesselingh F.P. SOLAR-FORCED 2600 BP AND LITTLE ICE AGE HIGHSTANDS OF THE CASPIAN SEA. South of Russia: ecology, development. 2008;3(4):15-25. (In Russ.) https://doi.org/10.18470/1992-1098-2008-4-15-25

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ISSN 1992-1098 (Print)
ISSN 2413-0958 (Online)