Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Kirill V. Chistyakov"'
Autor:
Dmitrii A. Ganyushkin, Sofia N. Lessovaia, Dmitrii Y. Vlasov, Gennady P. Kopitsa, László Almásy, Kirill V. Chistyakov, Elena G. Panova, Ekaterina Derkach, Anastasiya Alekseeva
Publikováno v:
Geosciences, Vol 11, Iss 8, p 342 (2021)
For the Altai Mountains’ region, especially the arid southeastern part of the Russian Altai, the data on glacier fluctuations in the Pleistocene and Holocene are still inconsistent. The study area was the Kargy River’s valley (2288–2387 m a.s.l
Externí odkaz:
https://doaj.org/article/060c9d7af52947e3a7e934696ba1f3bc
Autor:
Dmitry V. Bantcev, Dmitry A. Ganyushkin, Kirill V. Chistyakov, Ilya V. Volkov, Alexey A. Ekaykin, Arina N. Veres, Igor V. Tokarev, Natalya B. Shtykova, Tatiana A. Andreeva
Publikováno v:
Geosciences, Vol 9, Iss 7, p 297 (2019)
The aim of this study was to determine the contribution of snow and glacial ice to the river fluxes, and to identify the type of ice formation in the Tsambagarav massif (the northwestern part of Mongolia). The main method for this study was isotopic
Externí odkaz:
https://doaj.org/article/2d5a66cff12947a89ac0d2318c998be6
Autor:
Dmitry A. Ganyushkin, Kirill V. Chistyakov, Ilya V. Volkov, Dmitry V. Bantcev, Elena P. Kunaeva, Tatyana A. Andreeva, Anton V. Terekhov, Demberel Otgonbayar
Publikováno v:
Geosciences, Vol 8, Iss 11, p 414 (2018)
The Tavan Bogd mountains (of which, the main peak, Khuiten Uul, reaches 4374 m a.s.l.) are situated in the central part of the Altai mountain system, in the territories of Russia, Mongolia and China. The massif is the largest glacierized area of Alta
Externí odkaz:
https://doaj.org/article/8f4d2665129a42678130e2bda84c38d6
Autor:
Dmitry A. Ganyushkin, Kirill V. Chistyakov, Ilya V. Volkov, Dmitry V. Bantcev, Elena P. Kunaeva, Anton V. Terekhov
Publikováno v:
Geosciences, Vol 7, Iss 4, p 117 (2017)
This research is based on multiyear in-situ observations, analysis of satellite and aerial imagery, meteorological data, and mass balance index calculations. Presently, 659 glaciers cover a total area of 322.1 km2. We identified four favorable, two n
Externí odkaz:
https://doaj.org/article/77918e85696a40508c6788e44cdfc033