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Отложения приледниковых озёр – основа для создания непрерывных летописей истории голоценового оледенения
https://doi.org/10.15356/2076-6734-2015-1-89-102
Аннотация
Применение палеолимнологических методов в гляциологии даёт возможность делать непрерывные реконструкции высоты границы питания ледников, что невозможно никакими другими известными в настоящее время методами. Палеолимнологические методы позволяют также установить время исчезновения ледника из водосбора при его отступании в прошлом и время появления при активизации оледенения. Все эти сведения имеют важнейшее палеоклиматическое значение. Развитие комплекса палеолимнологических методов, их сочетание с другими методами палеогляциологии – приоритетные направления палеоклиматологии ввиду уникальности получаемой информации и возможности создания палеоклиматических реконструкций высокого разрешения
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Дополнительные файлы
Для цитирования: Александрин М.Ю. Отложения приледниковых озёр – основа для создания непрерывных летописей истории голоценового оледенения. Лёд и Снег. 2015;55(1):89-102. https://doi.org/10.15356/2076-6734-2015-1-89-102
For citation: Alexandrin M.Y. Proglacial lake sediments – a basis for uninterrupted chronicles of the Holocene glacier variations. Ice and Snow. 2015;55(1):89-102. (In Russ.) https://doi.org/10.15356/2076-6734-2015-1-89-102
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ISSN 2076-6734 (Print)
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