Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review
Black carbon is considered a product of the incomplete combustion of fossil fuels and materials that originated from volcanic eruptions or were emitted during wildfires. It is a strong light-absorbing component that has many atmospheric and surface effects in terrestrial and glacial ecosystems. Norm...
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fttomskstateuniv:vtls:000792880 2023-05-15T13:57:13+02:00 Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review Polyakov, Vyacheslav I. Abakumov, Evgeny V. Tembotov, Rustam Kh. 2020 application/pdf https://doi.org/10.17223/19988591/52/1 http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000792880 eng eng vtls:000792880 doi:10.17223/19988591/52/1 http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000792880 Вестник Томского государственного университета. Биология. 2020. № 52. С. 6-33 черный углерод Центральный Кавказ Арктика Антарктика климатический кризис статьи в журналах info:eu-repo/semantics/article 2020 fttomskstateuniv https://doi.org/10.17223/19988591/52/1 2021-02-09T17:29:21Z Black carbon is considered a product of the incomplete combustion of fossil fuels and materials that originated from volcanic eruptions or were emitted during wildfires. It is a strong light-absorbing component that has many atmospheric and surface effects in terrestrial and glacial ecosystems. Normally, black carbon is presented as a solid particle, consisting mainly of pure carbon, which absorbs solar radiation at all wavelengths. Some black carbon particles are amended by a mineral compound, though black carbon substances are normally dark or greyish dark. Black carbon is the most active part of suspended particles in the atmosphere and on glacial surfaces, absorbing solar radiation, the main component of ash, which consists of carbon particles with impurities in the form of mineral particles and also contains carbon of biogenic origin. In this paper, we have analyzed the literature on black carbon and its effect on deglaciation processes in the Earth’s polar and mountainous regions. The physical, chemical, and microbiological composition of black carbon accumulations were studied using the examples of the Arctic, the Antarctic, and the Central Caucasus. Potential sources and conditions of the transportation of black carbon into the polar zone and their effect on ice and snow have also been discussed. Article in Journal/Newspaper Antarc* Antarctic Arctic black carbon Антарктика Арктика Tomsk State University Research Library Arctic Antarctic The Antarctic Vestnik Tomskogo gosudarstvennogo universiteta. Biologiya 52 6 33 |
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Open Polar |
collection |
Tomsk State University Research Library |
op_collection_id |
fttomskstateuniv |
language |
English |
topic |
черный углерод Центральный Кавказ Арктика Антарктика климатический кризис |
spellingShingle |
черный углерод Центральный Кавказ Арктика Антарктика климатический кризис Polyakov, Vyacheslav I. Abakumov, Evgeny V. Tembotov, Rustam Kh. Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review |
topic_facet |
черный углерод Центральный Кавказ Арктика Антарктика климатический кризис |
description |
Black carbon is considered a product of the incomplete combustion of fossil fuels and materials that originated from volcanic eruptions or were emitted during wildfires. It is a strong light-absorbing component that has many atmospheric and surface effects in terrestrial and glacial ecosystems. Normally, black carbon is presented as a solid particle, consisting mainly of pure carbon, which absorbs solar radiation at all wavelengths. Some black carbon particles are amended by a mineral compound, though black carbon substances are normally dark or greyish dark. Black carbon is the most active part of suspended particles in the atmosphere and on glacial surfaces, absorbing solar radiation, the main component of ash, which consists of carbon particles with impurities in the form of mineral particles and also contains carbon of biogenic origin. In this paper, we have analyzed the literature on black carbon and its effect on deglaciation processes in the Earth’s polar and mountainous regions. The physical, chemical, and microbiological composition of black carbon accumulations were studied using the examples of the Arctic, the Antarctic, and the Central Caucasus. Potential sources and conditions of the transportation of black carbon into the polar zone and their effect on ice and snow have also been discussed. |
format |
Article in Journal/Newspaper |
author |
Polyakov, Vyacheslav I. Abakumov, Evgeny V. Tembotov, Rustam Kh. |
author_facet |
Polyakov, Vyacheslav I. Abakumov, Evgeny V. Tembotov, Rustam Kh. |
author_sort |
Polyakov, Vyacheslav I. |
title |
Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review |
title_short |
Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review |
title_full |
Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review |
title_fullStr |
Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review |
title_full_unstemmed |
Black carbon as a factor in deglaciation in polar and mountain ecosystems: A review |
title_sort |
black carbon as a factor in deglaciation in polar and mountain ecosystems: a review |
publishDate |
2020 |
url |
https://doi.org/10.17223/19988591/52/1 http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000792880 |
geographic |
Arctic Antarctic The Antarctic |
geographic_facet |
Arctic Antarctic The Antarctic |
genre |
Antarc* Antarctic Arctic black carbon Антарктика Арктика |
genre_facet |
Antarc* Antarctic Arctic black carbon Антарктика Арктика |
op_source |
Вестник Томского государственного университета. Биология. 2020. № 52. С. 6-33 |
op_relation |
vtls:000792880 doi:10.17223/19988591/52/1 http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000792880 |
op_doi |
https://doi.org/10.17223/19988591/52/1 |
container_title |
Vestnik Tomskogo gosudarstvennogo universiteta. Biologiya |
container_issue |
52 |
container_start_page |
6 |
op_container_end_page |
33 |
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1766264818359074816 |