Zobrazeno 1 - 10
of 43
pro vyhledávání: '"K. V. Chistyakov"'
Autor:
D. A. Ganyushkin, O. S. Konkova, K. V. Chistyakov, D. V. Bantcev, A. V. Terekhov, E. P. Kunaeva, Yu. N. Kurochkin, T. A. Andreeva, D. D. Volkova
Publikováno v:
Лëд и снег, Vol 61, Iss 4, Pp 500-520 (2021)
Based on the analysis of remote data and field observations, we reconstructed the glaciation of the Shapshal Center (Eastern Altai) for the maximum of the Little Ice Age (LIA) and by the state of the glaciers as of 2001. At the maximum of the LIA, gl
Externí odkaz:
https://doaj.org/article/d7fb83bf8fc34ac5b91d135b1788bca8
Autor:
D. A. Ganyushkin, O. S. Konkova, K. V. Chistyakov, A. A. Ekaykin, I. V. Volkov, D. V. Bantcev, A. V. Terekhov, E. P. Kunaeva, Yu. N. Kurochkin
Publikováno v:
Лëд и снег, Vol 61, Iss 1, Pp 38-57 (2021)
Catalogues and maps of glaciers (for 2015) of Shapshal Glacier Center, located in the eastern part of the Russian Altai, have been created based on the first field glaciological observations and space images interpretation. In total 123 glaciers with
Externí odkaz:
https://doaj.org/article/9393e1f031e24afa803e08f89eabed4d
Autor:
D. V. Bantsev, D. A. Ganyushkin, K. V. Chistyakov, A. A. Ekaykin, I. V. Tokarev, I. V. Volkov
Publikováno v:
Лëд и снег, Vol 58, Iss 3, Pp 333-342 (2018)
This investigation is based on measurements of stable isotopes concentrations (δD and δ18О) in water, snow and ice samples. Glaciers are composed of ice, snow, and fi n of atmospheric origin. The isotopic composition of these components is differe
Externí odkaz:
https://doaj.org/article/e41f507675d64ed4b0db244380141409
Autor:
D. A. Ganyushkin, K. V. Chistyakov, I. V. Volkov, D. V. Bantsev, E. P. Kunaeva, N. F. Kharlamova
Publikováno v:
Лëд и снег, Vol 57, Iss 3, Pp 307-325 (2017)
As of 2015, 16 glaciers, their total area 23.46 km2 and the weighted-mean altitude of the firn line 3335 m, were isolated on the Northern slope of the of the Tavan-Bogdo-Ola massif (Altai) on the basis of field studies and analysis of satellite image
Externí odkaz:
https://doaj.org/article/705e5ffce0024b648c99fd7419e4f8ea
Publikováno v:
Лëд и снег, Vol 56, Iss 4, Pp 437-452 (2016)
Characteristics of glacierization of the Tsambagarav mountain ridge were determined on the basis of images obtained from satellites Corona, Landsat‑5, Spot‑4, Landsat‑8 together with results of field investigations. Inventories of glaciers loca
Externí odkaz:
https://doaj.org/article/94a4a79540784f078fb6fc9e40864916
Publikováno v:
Лëд и снег, Vol 56, Iss 2, Pp 169-176 (2016)
Results of investigation of glacio-nival systems made in the Tabyn-Bogdo-Ola mountains (Western Mongolia) are presented in the paper. Average content of δ18О in the Tsagan-Us river water amounts to 17.44‰ that is almost equal to the isotope conte
Externí odkaz:
https://doaj.org/article/b22c986ceef64a33aec1cee5a8b5edb7
Publikováno v:
Лëд и снег, Vol 56, Iss 1, Pp 29-42 (2016)
Glaciation of the Chikhachev ridge (South-Eastern Altai) remains poorly known: field observations were not performed since the mid-twentieth century, available schemes and estimates of the glaciation and its scale made on the basis of remote sensing
Externí odkaz:
https://doaj.org/article/5fa993b54a8949219f851aff75547e26
Autor:
P. N. Svyashchennikov, A. V. Urazgildeeva, Y. N. Kurochkin, B. V. Ivanov, K. V. Chistyakov, D. Divin, S. Hudson
Publikováno v:
Лëд и снег, Vol 55, Iss 3, Pp 67-72 (2015)
Data on spectral composition of shortwave radiation that is reflected from snow and penetrates deep into the snow cover obtained near the Barentsburg settlement (Svalbard) are discussed in the paper. Measurements were made by the use of the spectral
Externí odkaz:
https://doaj.org/article/a906e9fb543f4c21898f101723f799ad
Publikováno v:
Лëд и снег, Vol 53, Iss 4, Pp 43-51 (2015)
The article is dedicated to perennial snow patches of Mongun-Taiga mountain massif (south-western Tuva), their morphology, present state and dynamics over the last 45 years. We created a scheme of snow patch classification with regard to genesis of r
Externí odkaz:
https://doaj.org/article/4e3af6443d4143389e52a35e065f209e
Publikováno v:
Лëд и снег, Vol 53, Iss 3, Pp 33-44 (2015)
Dynamics of glaciation of the northern slope of Tavan-Bogdo-Ola in the period of 1962–2011 has been defined on basis of field observations and analysis of aerial photos. Glaciers of the first and of the second Late Neopleistocene glaciations, histo
Externí odkaz:
https://doaj.org/article/7f7c3aca7a6446d0a4f5f7a6cb16b308