Change of Chalaati Glacier (Georgian Caucasus) since the Little Ice Age based on dendrochronological and Beryllium‑10 data

Change of Chalaati Glacier (Georgian Caucasus) since the Little Ice Age based on dendrochronological and Beryllium‑10 data

Glacier variations over the past centuries are still poorly documented on the southern slope of the Greater Caucasus. In this paper, the change of Chalaati Glacier in the Georgian Caucasus from its maximum extent during the Little Ice Age has been studied. For the first time in the history of glacio...

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Bibliografiske detaljer
Main Authors: L. G. Tielidze, O. N. Solomina, V. Jomelli, E. A. Dolgova, I. S. Bushueva, V. N. Mikhalenko, R. Brauche, Team ASTER
Format: Article
Sprog:Russian
Udgivet: Nauka 2020-08-01
Serier:Лëд и снег
Fag:
cosmic ray exposure dating
dendrochronology
glacier variation
greater caucasus
little ice age
Online adgang:https://ice-snow.igras.ru/jour/article/view/823

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https://ice-snow.igras.ru/jour/article/view/823

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