ИЗОТОПНО-ГИДРОЛОГИЧЕСКИЕ ИССЛЕДОВАНИЯ В БАССЕЙНЕ Р. ТАЛДУРА (ЮЖНО-ЧУЙСКИЙ ХРЕБЕТ, ЦЕНТРАЛЬНЫЙ АЛТАЙ)

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Представлены результаты изотопных исследований в долине р. Талдура. Определены изотопные характеристики льда ледника Некрасова и воды рек и ручьёв в середине сезона абляции. Показано преобладание ледникового питания на всём протяжении р. Талдура. Установлено, что талые воды менее крупного ледника Некрасова оказывают меньшее влияние на питание моренного оз. Таможенное по сравнению с влиянием талых вод ледника Большая Талдура на сток р. Талдура.

Об авторах

Д. В. Банцев

Санкт-Петербургский государственный университет

Автор, ответственный за переписку.
Email: bancev-d@yandex.ru
Россия, Санкт-Петербург

А. А. Овсепян

Санкт-Петербургский государственный университет

Email: bancev-d@yandex.ru
Россия, Санкт-Петербург

В. А. Распутина

Санкт-Петербургский государственный университет

Email: bancev-d@yandex.ru
Россия, Санкт-Петербург

А. В. Козачек

Санкт-Петербургский государственный университет; Арктический и Антарктический научно-исследовательский институт

Email: bancev-d@yandex.ru
Россия, Санкт-Петербург; Россия, Санкт-Петербург

К. Б. Чихачев

Санкт-Петербургский государственный университет; Арктический и Антарктический научно-исследовательский институт

Email: bancev-d@yandex.ru
Россия, Санкт-Петербург; Россия, Санкт-Петербург

Д. А. Ганюшкин

Санкт-Петербургский государственный университет

Email: bancev-d@yandex.ru
Россия, Санкт-Петербург

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