Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China

A risk assessment of vegetation zone responses to climate change was conducted using the classical Holdridge life zone model on the Loess Plateau of Northwest China. The results show that there are currently ten vegetation zones occurring on the Loess Plateau (1950–2000), including alvar desert, alp...

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Published in:Forests
Main Authors: Guoqing Li, Zhongming Wen, Ke Guo, Sheng Du
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2015
Subjects:
Online Access:https://doi.org/10.3390/f6062092
https://doaj.org/article/8ad9319445044763b265762060e0514e
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spelling ftdoajarticles:oai:doaj.org/article:8ad9319445044763b265762060e0514e 2023-05-15T18:40:03+02:00 Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China Guoqing Li Zhongming Wen Ke Guo Sheng Du 2015-06-01T00:00:00Z https://doi.org/10.3390/f6062092 https://doaj.org/article/8ad9319445044763b265762060e0514e EN eng MDPI AG http://www.mdpi.com/1999-4907/6/6/2092 https://doaj.org/toc/1999-4907 1999-4907 doi:10.3390/f6062092 https://doaj.org/article/8ad9319445044763b265762060e0514e Forests, Vol 6, Iss 6, Pp 2092-2108 (2015) vegetation zone climate change Holdridge life zone vegetation mapping Plant ecology QK900-989 article 2015 ftdoajarticles https://doi.org/10.3390/f6062092 2023-01-08T01:29:38Z A risk assessment of vegetation zone responses to climate change was conducted using the classical Holdridge life zone model on the Loess Plateau of Northwest China. The results show that there are currently ten vegetation zones occurring on the Loess Plateau (1950–2000), including alvar desert, alpine wet tundra, alpine rain tundra, boreal moist forest, boreal wet forest, cool temperate desert, cool temperate desert scrub, cool temperate steppe, cool temperate moist forest, warm temperate desert scrub, warm temperate thorn steppe, and warm temperate dry forest. Seventy years later (2070S), the alvar desert, the alpine wet tundra and the cool temperate desert will disappear, while warm temperate desert scrub and warm temperate thorn steppe will emerge. The area proportion of warm temperate dry forest will expand from 12.2% to 22.8%–37.2%, while that of cool temperate moist forest will decrease from 18.5% to 6.9%–9.5%. The area proportion of cool temperate steppe will decrease from 51.8% to 34.5%–51.6%. Our results suggest that future climate change will be conducive to the growth and expansion of forest zones on the Loess Plateau, which can provide valuable reference information for regional vegetation restoration planning and adaptive strategies in this region. Article in Journal/Newspaper Tundra Directory of Open Access Journals: DOAJ Articles Forests 6 12 2092 2108
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic vegetation zone
climate change
Holdridge life zone
vegetation mapping
Plant ecology
QK900-989
spellingShingle vegetation zone
climate change
Holdridge life zone
vegetation mapping
Plant ecology
QK900-989
Guoqing Li
Zhongming Wen
Ke Guo
Sheng Du
Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China
topic_facet vegetation zone
climate change
Holdridge life zone
vegetation mapping
Plant ecology
QK900-989
description A risk assessment of vegetation zone responses to climate change was conducted using the classical Holdridge life zone model on the Loess Plateau of Northwest China. The results show that there are currently ten vegetation zones occurring on the Loess Plateau (1950–2000), including alvar desert, alpine wet tundra, alpine rain tundra, boreal moist forest, boreal wet forest, cool temperate desert, cool temperate desert scrub, cool temperate steppe, cool temperate moist forest, warm temperate desert scrub, warm temperate thorn steppe, and warm temperate dry forest. Seventy years later (2070S), the alvar desert, the alpine wet tundra and the cool temperate desert will disappear, while warm temperate desert scrub and warm temperate thorn steppe will emerge. The area proportion of warm temperate dry forest will expand from 12.2% to 22.8%–37.2%, while that of cool temperate moist forest will decrease from 18.5% to 6.9%–9.5%. The area proportion of cool temperate steppe will decrease from 51.8% to 34.5%–51.6%. Our results suggest that future climate change will be conducive to the growth and expansion of forest zones on the Loess Plateau, which can provide valuable reference information for regional vegetation restoration planning and adaptive strategies in this region.
format Article in Journal/Newspaper
author Guoqing Li
Zhongming Wen
Ke Guo
Sheng Du
author_facet Guoqing Li
Zhongming Wen
Ke Guo
Sheng Du
author_sort Guoqing Li
title Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China
title_short Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China
title_full Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China
title_fullStr Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China
title_full_unstemmed Simulating the Effect of Climate Change on Vegetation Zone Distribution on the Loess Plateau, Northwest China
title_sort simulating the effect of climate change on vegetation zone distribution on the loess plateau, northwest china
publisher MDPI AG
publishDate 2015
url https://doi.org/10.3390/f6062092
https://doaj.org/article/8ad9319445044763b265762060e0514e
genre Tundra
genre_facet Tundra
op_source Forests, Vol 6, Iss 6, Pp 2092-2108 (2015)
op_relation http://www.mdpi.com/1999-4907/6/6/2092
https://doaj.org/toc/1999-4907
1999-4907
doi:10.3390/f6062092
https://doaj.org/article/8ad9319445044763b265762060e0514e
op_doi https://doi.org/10.3390/f6062092
container_title Forests
container_volume 6
container_issue 12
container_start_page 2092
op_container_end_page 2108
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