The results of 100-year-long observations of the glacial geosystem dynamics in the Munku-Sardyk massif

Китов, А. Д.; Коваленко, С. Н.; Plyusnin, V. M.

doi:10.1016/j.gnr.2009.09.012

Cited by 13 publications

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“…Those are 1897-1906, 1963, 1982, and 2006-2008. [13,14,50,51,54,55] According to these observations, the bottom bound of the glacier was lowest (Fig. 6).…”

Section: Reconstruction Of Peretolchin Glaciermentioning

confidence: 76%

Tracing recent glacial events in bottom sediments of a glacial lake (East Sayan Ridge, Russia) from high‐resolution SR‐XRF, ICP‐MS, and FTIR records

et al. 2015

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The paper presents a study of bottom sediments of proglacial Lake Ehoy, which intakes the meltwater of Peretolchin glacier, the East Sayan Ridge. A bottom sediment sequence that formed in the period of 1885-2013 was investigated with a year/season time resolution using X-ray fluorescence with synchrotron radiation and conventional analysis. A depth-age model of the core was based on counting of the annual laminae. The model was checked by an analysis of the distribution of activity of

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“…Those are 1897-1906, 1963, 1982, and 2006-2008. [13,14,50,51,54,55] According to these observations, the bottom bound of the glacier was lowest (Fig. 6).…”

Section: Reconstruction Of Peretolchin Glaciermentioning

confidence: 76%

Tracing recent glacial events in bottom sediments of a glacial lake (East Sayan Ridge, Russia) from high‐resolution SR‐XRF, ICP‐MS, and FTIR records

et al. 2015

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“…The Peretolchina glacier under the main summit of the Munku-Sardyk has shrunk significantly for the last 100 years (Kitov et al 2009). The area of the Northern Peretolchina glacier has decreased from 0.68 to 0.34 km 2 , according to other sources-to 0.3 km 2 (Osipov and Osipova 2014).…”

Section: Resultsmentioning

confidence: 99%

Nival-glacial dynamics of geosystems in Eastern Siberia (Russia) for the last 50 years

Китов

Plyusnin

2015

Environ Earth Sci

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It is presented the results of studying of small glaciers located in the Eastern Siberia along transect the Kodar mountains -Baikalskiy and Barguzinskiy ridgesthe Eastern Sayan mountains. Some glaciers from this transect have not been described before. The inventorying of these glaciers is based on high-resolution satellite images and fieldworks. The most numbers of glaciers are located in the Kodar mountains and few are in the Baikalskiy and the Barguzinskiy ridges. Most likely, these glaciers remained mainly due to coldest winters and geomorphologic features. The main parameters of a glacier's data (the dynamics, the current state, cartographic representation, remote sensing data and others) are selected by analogy of the international glaciological database.

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“…Данная работа представляет продолжение исследований геосистем горного массива Мунку-Сардык и их особенностей в связи с изменением климата [Kitov et al, 2009].…”

Section: по классификации галанинаunclassified

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ICIGIS

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The results of 100-year-long observations of the glacial geosystem dynamics in the Munku-Sardyk massif

Cited by 13 publications

References 0 publications

Tracing recent glacial events in bottom sediments of a glacial lake (East Sayan Ridge, Russia) from high‐resolution SR‐XRF, ICP‐MS, and FTIR records

Tracing recent glacial events in bottom sediments of a glacial lake (East Sayan Ridge, Russia) from high‐resolution SR‐XRF, ICP‐MS, and FTIR records

Nival-glacial dynamics of geosystems in Eastern Siberia (Russia) for the last 50 years

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