Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals
Shrub expansion into arctic and alpine tundra is one of the prominent vegetation changes currently underway. We studied the expansion of shrub vegetation into high elevation tundra in the Kvarkush Range of the Northern Ural mountains, Russia. Age structure analysis of the dominant shrubJuniperus sib...
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ftchinacadscimhe:oai:ir.imde.ac.cn:131551/50612 2023-05-15T15:07:28+02:00 Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals Grigoriev, Andrey A. Shalaumova, Yulia, V Erokhina, Olga, V Sokovnina, Svetlana Yu Vatolina, Elizaveta, I Wilmking, Martin 2020 http://ir.imde.ac.cn/handle/131551/50612 https://doi.org/10.1007/s11629-019-5925-6 英语 eng JOURNAL OF MOUNTAIN SCIENCE http://ir.imde.ac.cn/handle/131551/50612 doi:10.1007/s11629-019-5925-6 cn.org.cspace.api.content.CopyrightPolicy@1ef1c4f5 Juniperus sibirica Expansion Tundra Vegetation Plant communities Climate changes Northern Ural mountains Article 期刊论文 2020 ftchinacadscimhe https://doi.org/10.1007/s11629-019-5925-6 2022-12-19T18:27:45Z Shrub expansion into arctic and alpine tundra is one of the prominent vegetation changes currently underway. We studied the expansion of shrub vegetation into high elevation tundra in the Kvarkush Range of the Northern Ural mountains, Russia. Age structure analysis of the dominant shrubJuniperus sibiricaBurgsd. seems to support ongoing upslope advance of shrubs, a process particularly active in the second half of the 20(th)century. We found a close connection between the expansion of shrub vegetation and the general change in climatic conditions of the cold season (months with mean air temperature below 0 degrees C from November to March). In general, the greatest influence on the distribution ofJ. sibiricais exerted by the climate conditions of the beginning (November-January) and the end (March) of the cold season. With increasing elevation, the correlation coefficients between the establishment ofJ. sibiricashrubs and the precipitation of the beginning of the cold season increased, and reached maximum values at the top elevation level of the study area. However, the upwards shift ofJ. sibiricainto typical mountain tundra does not lead to changes in the ecological structure of vegetation at this stage, but simply a decrease in the area of mountain tundra. Article in Journal/Newspaper Arctic Climate change Tundra ural mountains IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences) Arctic Journal of Mountain Science 17 10 2339 2353 |
institution |
Open Polar |
collection |
IMHE OpenIR (Institute of Mountain Hazards and Environment, Chinese Academy of Sciences) |
op_collection_id |
ftchinacadscimhe |
language |
English |
topic |
Juniperus sibirica Expansion Tundra Vegetation Plant communities Climate changes Northern Ural mountains |
spellingShingle |
Juniperus sibirica Expansion Tundra Vegetation Plant communities Climate changes Northern Ural mountains Grigoriev, Andrey A. Shalaumova, Yulia, V Erokhina, Olga, V Sokovnina, Svetlana Yu Vatolina, Elizaveta, I Wilmking, Martin Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals |
topic_facet |
Juniperus sibirica Expansion Tundra Vegetation Plant communities Climate changes Northern Ural mountains |
description |
Shrub expansion into arctic and alpine tundra is one of the prominent vegetation changes currently underway. We studied the expansion of shrub vegetation into high elevation tundra in the Kvarkush Range of the Northern Ural mountains, Russia. Age structure analysis of the dominant shrubJuniperus sibiricaBurgsd. seems to support ongoing upslope advance of shrubs, a process particularly active in the second half of the 20(th)century. We found a close connection between the expansion of shrub vegetation and the general change in climatic conditions of the cold season (months with mean air temperature below 0 degrees C from November to March). In general, the greatest influence on the distribution ofJ. sibiricais exerted by the climate conditions of the beginning (November-January) and the end (March) of the cold season. With increasing elevation, the correlation coefficients between the establishment ofJ. sibiricashrubs and the precipitation of the beginning of the cold season increased, and reached maximum values at the top elevation level of the study area. However, the upwards shift ofJ. sibiricainto typical mountain tundra does not lead to changes in the ecological structure of vegetation at this stage, but simply a decrease in the area of mountain tundra. |
format |
Article in Journal/Newspaper |
author |
Grigoriev, Andrey A. Shalaumova, Yulia, V Erokhina, Olga, V Sokovnina, Svetlana Yu Vatolina, Elizaveta, I Wilmking, Martin |
author_facet |
Grigoriev, Andrey A. Shalaumova, Yulia, V Erokhina, Olga, V Sokovnina, Svetlana Yu Vatolina, Elizaveta, I Wilmking, Martin |
author_sort |
Grigoriev, Andrey A. |
title |
Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals |
title_short |
Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals |
title_full |
Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals |
title_fullStr |
Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals |
title_full_unstemmed |
Expansion ofJuniperus sibiricaBurgsd. as a response to climate change and associated effect on mountain tundra vegetation in the Northern Urals |
title_sort |
expansion ofjuniperus sibiricaburgsd. as a response to climate change and associated effect on mountain tundra vegetation in the northern urals |
publishDate |
2020 |
url |
http://ir.imde.ac.cn/handle/131551/50612 https://doi.org/10.1007/s11629-019-5925-6 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change Tundra ural mountains |
genre_facet |
Arctic Climate change Tundra ural mountains |
op_relation |
JOURNAL OF MOUNTAIN SCIENCE http://ir.imde.ac.cn/handle/131551/50612 doi:10.1007/s11629-019-5925-6 |
op_rights |
cn.org.cspace.api.content.CopyrightPolicy@1ef1c4f5 |
op_doi |
https://doi.org/10.1007/s11629-019-5925-6 |
container_title |
Journal of Mountain Science |
container_volume |
17 |
container_issue |
10 |
container_start_page |
2339 |
op_container_end_page |
2353 |
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1766338961455710208 |