Сокращение ледников Южно-Чуйского хребта (Алтай) с максимума малого ледникового периода

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Реконструированы и каталогизированы ледники Южно-Чуйского хребта в малый ледниковый период, в 1962, 2000 и 2021 гг. C максимума МЛП по 2021 г. суммарная площадь ледников сократилась на 61% и объём на 59–64%. Нижний предел распространения ледников поднялся на 300 м, максимум распределения льда по высоте – на 100 м. Сокращение площади ледников в 2000–2021 гг. ускорилось до 1.5% в год от площади на начало этапа.

Об авторах

Д. А. Ганюшкин

Санкт-Петербургский государственный университет

Автор, ответственный за переписку.
Email: d.ganyushkin@spbu.ru
Россия, Санкт-Петербург

Д. В. Банцев

Санкт-Петербургский государственный университет

Email: d.ganyushkin@spbu.ru
Россия, Санкт-Петербург

С. А. Грига

Санкт-Петербургский государственный университет

Email: d.ganyushkin@spbu.ru
Россия, Санкт-Петербург

Е. С. Деркач

Санкт-Петербургский государственный университет

Email: d.ganyushkin@spbu.ru
Россия, Санкт-Петербург

О. В. Останин

Алтайский государственный университет

Email: d.ganyushkin@spbu.ru
Россия, Барнаул

Ю. А. Горбунова

Санкт-Петербургский государственный университет

Email: d.ganyushkin@spbu.ru
Россия, Санкт-Петербург

В. А. Распутина

Санкт-Петербургский государственный университет

Email: d.ganyushkin@spbu.ru
Россия, Санкт-Петербург

К. В. Чистяков

Санкт-Петербургский государственный университет

Email: d.ganyushkin@spbu.ru
Россия, Санкт-Петербург

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