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: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2015
Subjects:
Online Access:https://doi.org/10.3390/f6062092
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spelling ftmdpi:oai:mdpi.com:/1999-4907/6/6/2092/ 2023-08-20T04:10:13+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 agris 2015-06-11 application/pdf https://doi.org/10.3390/f6062092 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/f6062092 https://creativecommons.org/licenses/by/4.0/ Forests; Volume 6; Issue 6; Pages: 2092-2108 vegetation zone climate change Holdridge life zone vegetation mapping Text 2015 ftmdpi https://doi.org/10.3390/f6062092 2023-07-31T20:44:18Z 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. Text Tundra MDPI Open Access Publishing Forests 6 12 2092 2108
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic vegetation zone
climate change
Holdridge life zone
vegetation mapping
spellingShingle vegetation zone
climate change
Holdridge life zone
vegetation mapping
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
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 Text
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 Multidisciplinary Digital Publishing Institute
publishDate 2015
url https://doi.org/10.3390/f6062092
op_coverage agris
genre Tundra
genre_facet Tundra
op_source Forests; Volume 6; Issue 6; Pages: 2092-2108
op_relation https://dx.doi.org/10.3390/f6062092
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/f6062092
container_title Forests
container_volume 6
container_issue 12
container_start_page 2092
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