Search Results - "Ganyushkin, D. A."
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Features of the Level Regime of Periglacial Moraine-Dammed Lakes in the Growth Stage (Based on the Example of Lakes of the Tavan–Bogdo–Ola Mountain Range, South Eastern Altai)
Published in Water resources (01-12-2023)“…The features of the hydrological regime of two periglacial lakes with a transgressive development phase, located on the Tavan–Bogdo–Ola mountain range in the…”
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The Use of Isotope Indicators in Hydrological Studies in the Taldura River Basin, Central Altai
Published in Lëd i sneg (01-01-2024)“…Received June 29, 2023; revised August 28, 2023; accepted October 2, 2023Stable isotopes investigation was carried out in the territory of the Yuzhno-Chuya…”
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Thickness and Volume of Glaciers of the Mongun-taiga Massif, Altai, in 2021 Based on Ground Penetrating Radar Data and Modeling
Published in Lëd i sneg (01-01-2024)“…Received April 26, 2023; revised August 18, 2023; accepted October 2, 2023This article presents the results of estimating the scale of the present-day…”
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The water level regime of periglacial lakes during the growth stage (the lakes of the Tavan-Bogdo-Ola mountain massif, South-Eastern Altai)
Published in Lëd i sneg (01-09-2022)“…Assessment of the dynamics of high-altitude glacial lakes is becoming increasingly important in the context of modern climate instability. The formation of new…”
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5
Shrinkage of Glaciers in Eastern Altai (Shapshal Center) after the Little Ice Age Maximum
Published in Water resources (01-12-2022)“…Glaciers of the little-studied Shapshal Glaciation Center in Eastern Altai during the Little Ice Age maximum have been reconstructed and the pattern of their…”
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Influence of the 1988 earthquake on glacierization and relief of the Tsambagarav massif (Western Mongolia)
Published in Lëd i sneg (01-02-2022)“…Early documentation of the consequences of the Tsambagarav earthquake happened on July 23, 1988 (M = 6.4) compiled by Soviet and Mongolian specialists allowed…”
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Shrinking of the glaciers of East Altai (Shapshal Center) after the maximum of the Little Ice Age
Published in Lëd i sneg (01-12-2021)“…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…”
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Interpretation of Glaciogenic Complexes From Satellite Images of the Mongun-Taiga Mountain Range
Published in Geography and natural resources (2018)“…This investigation is concerned with the problem of recognition of glacial landforms in arid mountainous areas of Asia using satellite imagery. We examine the…”
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The state of the Shapshalsky glacierization center (Eastern Altai) in 2015
Published in Lëd i sneg (25-03-2021)“…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…”
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Recent glacierization of the Tsambagarav ridge (North‑Western Mongolia) and its changes since the Little Ice Age maximum
Published in Lëd i sneg (21-12-2016)“…Characteristics of glacierization of the Tsambagarav mountain ridge were determined on the basis of images obtained from satellites Corona, Landsat‑5, Spot‑4,…”
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Formation of glacier runoff on the northern slope of Tavan Bogd mountain massif based on stable isotopes data
Published in Lëd i sneg (26-09-2018)“…This investigation is based on measurements of stable isotopes concentrations (δD and δ 18 О) in water, snow and ice samples. Glaciers are composed of ice,…”
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Modern data on glaciation of the northern slope of Tavan-Bogdo-Ola massif (Altai)
Published in Lëd i sneg (01-01-2017)“…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…”
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Isotope-geochemical investigation of glacio-nival systems of the Tabyn-Bogdo-Ola mountain massif (Western Mongolia)
Published in Lëd i sneg (11-05-2016)“…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…”
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14
Current glaciation of the Chikhachev ridge (South-Eastern Altai) and its dynamics after maximum of the Little Ice Age
Published in Lëd i sneg (17-02-2016)“…Glaciation of the Chikhachev ridge (South-Eastern Altai) remains poorly known: field observations were not performed since the mid-twentieth century, available…”
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15
Features of change of permanent snow patches in the Mongun-Taiga Massif, 1966–2011
Published in Lëd i sneg (06-04-2015)“…The article is dedicated to perennial snow patches of Mongun-Taiga mountain massif (south-western Tuva), their morphology, present state and dynamics over the…”
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Modern and ancient glaciation of northern slope of the Tavan-Bogdo-Ola massif
Published in Lëd i sneg (02-04-2015)“…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…”
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Present state and dynamics of glacio-nival systems of Mongun-Taiga and Tavan-Bogdo-Ola mountain massifs
Published in Lëd i sneg (01-03-2015)“…Climate-induced variations of glacio-nival systems (snow patches, glaciers, stone-ice formations) of the high-mountain massifs Mongun-Taiga and Tavan-Bogdo-Ola…”
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The outburst of dammed lake Maashey (North-Chuya ridge, Central Altai)
Published in Lëd i sneg (04-11-2024)“…The dammed lakes are widespread in mountainous areas and usually occur when river flow is blocked by landslides, rock glaciers, etc. Among such lakes, the most…”
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ОСОБЕННОСТИ УРОВЕННОГО РЕЖИМА ПРИЛЕДНИКОВЫХ МОРЕННО-ПОДПРУДНЫХ ОЗЁР В СТАДИИ РОСТА (НА ПРИМЕРЕ ОЗЁР ГОРНОГО МАССИВА ТАВАН-БОГДО-ОЛА, ЮГО-ВОСТОЧНЫЙ АЛТАЙ)
Published in Lëd i sneg (01-03-2022)Get full text
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ВЛИЯНИЕ ЗЕМЛЕТРЯСЕНИЯ 1988 Г. НА ОЛЕДЕНЕНИЕ И РЕЛЬЕФ МАССИВА ЦАМБАГАРАВ (ЗАПАДНАЯ МОНГОЛИЯ)
Published in Lëd i sneg (2022)Get full text
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