The thermal regime of soils in the north of Western Siberia
Abstract The results of long‐term stationary observations upon the thermal regime of soils in natural and anthropogenically‐disturbed tundra and northern taiga landscapes in the north of Western Siberia are discussed. Quantitative assessments of the heating effect of snow cover and the cooling effec...
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crwiley:10.1002/ppp.409 2024-06-02T08:13:04+00:00 The thermal regime of soils in the north of Western Siberia Pavlov, A. V. Moskalenko, N. G. 2002 http://dx.doi.org/10.1002/ppp.409 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.409 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.409 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 13, issue 1, page 43-51 ISSN 1045-6740 1099-1530 journal-article 2002 crwiley https://doi.org/10.1002/ppp.409 2024-05-03T11:50:26Z Abstract The results of long‐term stationary observations upon the thermal regime of soils in natural and anthropogenically‐disturbed tundra and northern taiga landscapes in the north of Western Siberia are discussed. Quantitative assessments of the heating effect of snow cover and the cooling effect of surface organic layer on soil temperatures in both winter and summer seasons are given. Spatial and temporal variations in the depth of seasonal thaw and soil temperatures in the tundra and taiga zones are outlined. Data on changes in soil temperature regimes following disturbance of surface organic layers are presented. Contemporary tendencies in permafrost degradation induced by climatic warming, changes in the snow cover depth, and anthropogenic impacts are shown. Copyright © 2002 John Wiley & Sons, Ltd. Article in Journal/Newspaper permafrost Permafrost and Periglacial Processes taiga Tundra Siberia Wiley Online Library Permafrost and Periglacial Processes 13 1 43 51 |
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English |
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Abstract The results of long‐term stationary observations upon the thermal regime of soils in natural and anthropogenically‐disturbed tundra and northern taiga landscapes in the north of Western Siberia are discussed. Quantitative assessments of the heating effect of snow cover and the cooling effect of surface organic layer on soil temperatures in both winter and summer seasons are given. Spatial and temporal variations in the depth of seasonal thaw and soil temperatures in the tundra and taiga zones are outlined. Data on changes in soil temperature regimes following disturbance of surface organic layers are presented. Contemporary tendencies in permafrost degradation induced by climatic warming, changes in the snow cover depth, and anthropogenic impacts are shown. Copyright © 2002 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Pavlov, A. V. Moskalenko, N. G. |
spellingShingle |
Pavlov, A. V. Moskalenko, N. G. The thermal regime of soils in the north of Western Siberia |
author_facet |
Pavlov, A. V. Moskalenko, N. G. |
author_sort |
Pavlov, A. V. |
title |
The thermal regime of soils in the north of Western Siberia |
title_short |
The thermal regime of soils in the north of Western Siberia |
title_full |
The thermal regime of soils in the north of Western Siberia |
title_fullStr |
The thermal regime of soils in the north of Western Siberia |
title_full_unstemmed |
The thermal regime of soils in the north of Western Siberia |
title_sort |
thermal regime of soils in the north of western siberia |
publisher |
Wiley |
publishDate |
2002 |
url |
http://dx.doi.org/10.1002/ppp.409 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.409 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.409 |
genre |
permafrost Permafrost and Periglacial Processes taiga Tundra Siberia |
genre_facet |
permafrost Permafrost and Periglacial Processes taiga Tundra Siberia |
op_source |
Permafrost and Periglacial Processes volume 13, issue 1, page 43-51 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.409 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
13 |
container_issue |
1 |
container_start_page |
43 |
op_container_end_page |
51 |
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1800759716680302592 |