Unique Surges of Medvezhy Glacier


Дәйексөз келтіру

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Аннотация

The results of 20 years of field data (1963–1982) and 50 years of remote observations (1963–2012) on Medvezhy Glacier in the Pamirs by the Institute of Geography, Russian Academy of Sciences, are considered. The prevalence of the influence of climatic factors over internal ones (features of ice deformation) on glacial surges is shown. A conclusion is made about the uniqueness of the surge regime of Medvezhy Glacier connected with the structure of its bed. There are no analogues of this structure of the bed on any of the 82 surging glaciers in the Pamirs.

Авторлар туралы

V. Kotlyakov

Institute of Geography, Russian Academy of Science

Email: tkhromova@gmail.com
Ресей, Moscow, 119017

L. Chernova

Institute of Geography, Russian Academy of Science

Email: tkhromova@gmail.com
Ресей, Moscow, 119017

T. Khromova

Institute of Geography, Russian Academy of Science

Хат алмасуға жауапты Автор.
Email: tkhromova@gmail.com
Ресей, Moscow, 119017

A. Muraviev

Institute of Geography, Russian Academy of Science

Email: tkhromova@gmail.com
Ресей, Moscow, 119017

A. Kachalin

Institute of Geography, Russian Academy of Science

Email: tkhromova@gmail.com
Ресей, Moscow, 119017

A. Tiuflin

Institute of Geography, Russian Academy of Science

Email: tkhromova@gmail.com
Ресей, Moscow, 119017

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