Zobrazeno 1 - 9
of 9
pro vyhledávání: '"I. S. Bushueva"'
Publikováno v:
Лëд и снег, Vol 63, Iss 3, Pp 410-425 (2023)
We present 11 10Be ages of the moraines of the Irik and Kashkatash glaciers that allowed identifying and dating several Late Holocene glacier advances for the first time, including a prominent advance exceeding the Little Ice Age (LIA) maximum that o
Externí odkaz:
https://doaj.org/article/32c5ef9d499e473d99e551ea84ce71f5
Publikováno v:
Лëд и снег, Vol 61, Iss 2, Pp 271-290 (2021)
Basing on treering analysis of more than 150pines growing in the Azau clearing, the minimum age of the deposits created by the Greater Azau Glacier was identified. Historical evidence, cartographic data, remote sensing materials, as well as the re
Externí odkaz:
https://doaj.org/article/52cf8677c3d24aaeabb9480a7ba9cf82
Autor:
L. G. Tielidze, O. N. Solomina, V. Jomelli, E. A. Dolgova, I. S. Bushueva, V. N. Mikhalenko, R. Brauche, Team ASTER
Publikováno v:
Лëд и снег, Vol 60, Iss 3, Pp 453-470 (2020)
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 st
Externí odkaz:
https://doaj.org/article/9d9d414926b346f68c26b9700c8e4a06
Publikováno v:
Лëд и снег, Vol 58, Iss 4, Pp 448-461 (2018)
On the basis of dendrochronological, lichenometric and historical data with the use of Earth remote sensing materials, the evolution of the Donguz-Orun Glacier has been reconstructed over the past centuries. In this work we used aerial photographs of
Externí odkaz:
https://doaj.org/article/1b15ba4d5568458787282910ad09639f
Publikováno v:
Лëд и снег, Vol 58, Iss 3, Pp 293-306 (2018)
The glaciers and ice caps in the Arctic are experiencing noticeable changes which are manifested, in particular, in the intensification of their dynamic instability. In this paper we present data on a largescale surge in the Western basin of the Vavi
Externí odkaz:
https://doaj.org/article/64628e10abe0475f94344a249537b880
Autor:
I. S. Bushueva, O. N. Solomina
Publikováno v:
Лëд и снег, Vol 52, Iss 2, Pp 121-130 (2015)
We focused our study on the retreat of a typical valley glacier Kashkatash, located in the Elbrus Area. We compared the old photographs of the glacier forefields (H. Burmester, 1911; H. Altberg, 1927; E.N. Lukasheva, 1932; unknown author, 1939) with
Externí odkaz:
https://doaj.org/article/461bcee33d9a46878f1ceb2bfd203c03
Publikováno v:
Лëд и снег, Vol 55, Iss 3, Pp 97-106 (2015)
In this article we present the reconstruction of fluctuations of Alibek valley glacier situated in the Teberda valley, Western Caucasus. The former positions of glacier of the past 120 years were reconstructed basing on the old photographs of 1904, 1
Externí odkaz:
https://doaj.org/article/699edc086af24c339138cd08db132418
Publikováno v:
Лëд и снег, Vol 52, Iss 1, Pp 85-94 (2015)
Using instrumental archives, aerial photographs, satellite images, old maps, descriptions of early explorers and old photographs we identified and mapped nine front positions of the Ullukam Glacier (SW slope of Elbrus) for the period from the end of
Externí odkaz:
https://doaj.org/article/4e237ca8bec84b469fc4aa0eba7601f8
Autor:
O. N. Solomina, P. A. Kalugin, M. Yu. Aleksandrin, I. S. Bushueva, A. V. Darin, E. A. Dolgova, V. Jomelli, M. N. Ivanov, V. V. Matskovsky, D. V. Ovchinnikov, I. O. Pavlolva, L. V. Razumovsky, A. A. Chepurnaya
Publikováno v:
Лëд и снег, Vol 53, Iss 2, Pp 102-111 (2015)
Lacustrine sediments represent an important data source for glacial and palaeoclimatic reconstructions. Having a number of certain advantages, they can be successfully used as a means of specification of glacier situation and age of moraine deposits,
Externí odkaz:
https://doaj.org/article/f4d0143be5c64f18ad9861e1724ecdce