Analysis of the pattern change process of Changbai Mountain wind-damaged landscape in the past thirty years

The wind-damaged landscape formed by the 1986 typhoon in Changbai Mountain Nature Reserve was studied in this paper. High-definition remote sensing images in 1987, 1993, 1999, 2004, 2010 and 2016 were selected to decode to analyze the change of each patch type in the study area. Fragstats 4.2 was us...

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Veröffentlicht in:Sheng tai xue bao 2022-08, Vol.42 (4), p.1327
Hauptverfasser: Chen, Xueying, Gao, Xuejiao, Xu, Jiawei, Jin, Yinghua, Zhang, Yingjie, Wang, Cailing
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container_title Sheng tai xue bao
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Gao, Xuejiao
Xu, Jiawei
Jin, Yinghua
Zhang, Yingjie
Wang, Cailing
description The wind-damaged landscape formed by the 1986 typhoon in Changbai Mountain Nature Reserve was studied in this paper. High-definition remote sensing images in 1987, 1993, 1999, 2004, 2010 and 2016 were selected to decode to analyze the change of each patch type in the study area. Fragstats 4.2 was used to quantitatively analyze the landscape pattern indices, and a combination of principal component analysis and comprehensive landscape evaluation index was used to make a comprehensive evaluation to reveal the process of landscape pattern changes 30 years after the wind damage. The results were as follows:(1) the dominance of herbaceous-shrub kept decreasing, but the distribution was homogenous, the patch shape was regular, and the degree of aggregation was high; broad-leaved forest and coniferous forest firstly increased in large patches during the recovery process, and later on the area increase was mainly in small patches, the patch shape of broad-leaved forest tended to be regular, and coniferous forest was complex; Betula ermanii forest firstly increased in small patches, and later on the large patches grew in succession, the shape became more complicated, and there was a trend of contiguous growth.(2) At the landscape level, small and scattered patches were converted into large and concentrated patches in the restoration process, the irregularity of shape increased and the connectivity of the landscape decreased. As the restoration continues, the landscape tended to be homogenized.(3) According to the landscape transfer matrix, herbaceous-shrub patches in the study area would be continuously transformed into arboreal patches, the proportion of herbaceous-shrub gradually decreased, while arboreal increased. Among them, herbaceous-shrub mainly transformed into broad-leaved forest, broad-leaved forest mainly transformed into coniferous forest, and coniferous forest mainly transformed into Betula ermanii forest. The four patch types of herbaceous-shrub, broad-leaved forest, coniferous forest, and Betula ermanii forest showed a succession relationship during the restoration process.(4) Through the principal component analysis method, two principal components related to landscape scale and shape and landscape dispersion, respectively, were identified as key indices to characterize landscape restoration.(5) Using the combination of principal component analysis and the comprehensive landscape evaluation index to evaluate the wind-damaged landscape in Changbai M
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High-definition remote sensing images in 1987, 1993, 1999, 2004, 2010 and 2016 were selected to decode to analyze the change of each patch type in the study area. Fragstats 4.2 was used to quantitatively analyze the landscape pattern indices, and a combination of principal component analysis and comprehensive landscape evaluation index was used to make a comprehensive evaluation to reveal the process of landscape pattern changes 30 years after the wind damage. The results were as follows:(1) the dominance of herbaceous-shrub kept decreasing, but the distribution was homogenous, the patch shape was regular, and the degree of aggregation was high; broad-leaved forest and coniferous forest firstly increased in large patches during the recovery process, and later on the area increase was mainly in small patches, the patch shape of broad-leaved forest tended to be regular, and coniferous forest was complex; Betula ermanii forest firstly increased in small patches, and later on the large patches grew in succession, the shape became more complicated, and there was a trend of contiguous growth.(2) At the landscape level, small and scattered patches were converted into large and concentrated patches in the restoration process, the irregularity of shape increased and the connectivity of the landscape decreased. As the restoration continues, the landscape tended to be homogenized.(3) According to the landscape transfer matrix, herbaceous-shrub patches in the study area would be continuously transformed into arboreal patches, the proportion of herbaceous-shrub gradually decreased, while arboreal increased. Among them, herbaceous-shrub mainly transformed into broad-leaved forest, broad-leaved forest mainly transformed into coniferous forest, and coniferous forest mainly transformed into Betula ermanii forest. The four patch types of herbaceous-shrub, broad-leaved forest, coniferous forest, and Betula ermanii forest showed a succession relationship during the restoration process.(4) Through the principal component analysis method, two principal components related to landscape scale and shape and landscape dispersion, respectively, were identified as key indices to characterize landscape restoration.(5) Using the combination of principal component analysis and the comprehensive landscape evaluation index to evaluate the wind-damaged landscape in Changbai Mountain, the results showed that during the 30-year restoration period, the quality of the study area was improved, but the recovery was slow and still differed significantly from that before the wind damage.(6) Multiple strong wind disturbances can form a non-standard vertical band spectrum on the western and southern slopes of Changbai Mountain.</description><identifier>ISSN: 1000-0933</identifier><identifier>DOI: 10.5846/stxb202101290316</identifier><language>chi ; eng</language><publisher>Beijing: Science Press</publisher><subject>Betula ermanii ; Coniferous forests ; Forests ; High definition ; Mountains ; Nature reserves ; Patches (structures) ; Pattern analysis ; Principal components analysis ; Recovery ; Remote sensing ; Restoration ; Transfer matrices ; Typhoons ; Wind ; Wind damage</subject><ispartof>Sheng tai xue bao, 2022-08, Vol.42 (4), p.1327</ispartof><rights>Copyright Science Press Aug 2022</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>315,782,786,27931,27932</link.rule.ids></links><search><creatorcontrib>Chen, Xueying</creatorcontrib><creatorcontrib>Gao, Xuejiao</creatorcontrib><creatorcontrib>Xu, Jiawei</creatorcontrib><creatorcontrib>Jin, Yinghua</creatorcontrib><creatorcontrib>Zhang, Yingjie</creatorcontrib><creatorcontrib>Wang, Cailing</creatorcontrib><title>Analysis of the pattern change process of Changbai Mountain wind-damaged landscape in the past thirty years</title><title>Sheng tai xue bao</title><description>The wind-damaged landscape formed by the 1986 typhoon in Changbai Mountain Nature Reserve was studied in this paper. High-definition remote sensing images in 1987, 1993, 1999, 2004, 2010 and 2016 were selected to decode to analyze the change of each patch type in the study area. Fragstats 4.2 was used to quantitatively analyze the landscape pattern indices, and a combination of principal component analysis and comprehensive landscape evaluation index was used to make a comprehensive evaluation to reveal the process of landscape pattern changes 30 years after the wind damage. The results were as follows:(1) the dominance of herbaceous-shrub kept decreasing, but the distribution was homogenous, the patch shape was regular, and the degree of aggregation was high; broad-leaved forest and coniferous forest firstly increased in large patches during the recovery process, and later on the area increase was mainly in small patches, the patch shape of broad-leaved forest tended to be regular, and coniferous forest was complex; Betula ermanii forest firstly increased in small patches, and later on the large patches grew in succession, the shape became more complicated, and there was a trend of contiguous growth.(2) At the landscape level, small and scattered patches were converted into large and concentrated patches in the restoration process, the irregularity of shape increased and the connectivity of the landscape decreased. As the restoration continues, the landscape tended to be homogenized.(3) According to the landscape transfer matrix, herbaceous-shrub patches in the study area would be continuously transformed into arboreal patches, the proportion of herbaceous-shrub gradually decreased, while arboreal increased. Among them, herbaceous-shrub mainly transformed into broad-leaved forest, broad-leaved forest mainly transformed into coniferous forest, and coniferous forest mainly transformed into Betula ermanii forest. The four patch types of herbaceous-shrub, broad-leaved forest, coniferous forest, and Betula ermanii forest showed a succession relationship during the restoration process.(4) Through the principal component analysis method, two principal components related to landscape scale and shape and landscape dispersion, respectively, were identified as key indices to characterize landscape restoration.(5) Using the combination of principal component analysis and the comprehensive landscape evaluation index to evaluate the wind-damaged landscape in Changbai Mountain, the results showed that during the 30-year restoration period, the quality of the study area was improved, but the recovery was slow and still differed significantly from that before the wind damage.(6) Multiple strong wind disturbances can form a non-standard vertical band spectrum on the western and southern slopes of Changbai Mountain.</description><subject>Betula ermanii</subject><subject>Coniferous forests</subject><subject>Forests</subject><subject>High definition</subject><subject>Mountains</subject><subject>Nature reserves</subject><subject>Patches (structures)</subject><subject>Pattern analysis</subject><subject>Principal components analysis</subject><subject>Recovery</subject><subject>Remote sensing</subject><subject>Restoration</subject><subject>Transfer matrices</subject><subject>Typhoons</subject><subject>Wind</subject><subject>Wind damage</subject><issn>1000-0933</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNpdUMtOwzAQ9AEkyuPO0RLnwG42TpNjVfGSirj0Hm1sp01pnWK7gvw9LuXEZV8zGu2MELcI96oqyocQv9sccgTMayAsz8QEASCDmuhCXIawASBAqifiY-Z4O4Y-yKGTcW3lnmO03km9ZrdKqx-0Db_o_HhpuZdvw8FF7p386p3JDO94ZY3csjNB897KhJyUQkxD7-MoR8s-XIvzjrfB3vz1K7F8elzOX7LF-_PrfLbIdFlTKnnBUJQtKE0wrauiqytismi0soXCZJGxUliDtmxy1FCBJqNw2mpVAF2Ju5Ns-v3zYENsNsPBJ5uhyafJeIWKKLHgxNJ-CMHbrtn7fsd-bBCaY4rN_xTpBzYFZ8g</recordid><startdate>20220801</startdate><enddate>20220801</enddate><creator>Chen, Xueying</creator><creator>Gao, Xuejiao</creator><creator>Xu, Jiawei</creator><creator>Jin, Yinghua</creator><creator>Zhang, Yingjie</creator><creator>Wang, Cailing</creator><general>Science Press</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7SN</scope><scope>7ST</scope><scope>7UA</scope><scope>C1K</scope><scope>SOI</scope></search><sort><creationdate>20220801</creationdate><title>Analysis of the pattern change process of Changbai Mountain wind-damaged landscape in the past thirty years</title><author>Chen, Xueying ; Gao, Xuejiao ; Xu, Jiawei ; Jin, Yinghua ; Zhang, Yingjie ; Wang, Cailing</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c693-c624a046b05c307984f983a3e1dc5e451584a185190cead21c080c3d517bc5403</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi ; eng</language><creationdate>2022</creationdate><topic>Betula ermanii</topic><topic>Coniferous forests</topic><topic>Forests</topic><topic>High definition</topic><topic>Mountains</topic><topic>Nature reserves</topic><topic>Patches (structures)</topic><topic>Pattern analysis</topic><topic>Principal components analysis</topic><topic>Recovery</topic><topic>Remote sensing</topic><topic>Restoration</topic><topic>Transfer matrices</topic><topic>Typhoons</topic><topic>Wind</topic><topic>Wind damage</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chen, Xueying</creatorcontrib><creatorcontrib>Gao, Xuejiao</creatorcontrib><creatorcontrib>Xu, Jiawei</creatorcontrib><creatorcontrib>Jin, Yinghua</creatorcontrib><creatorcontrib>Zhang, Yingjie</creatorcontrib><creatorcontrib>Wang, Cailing</creatorcontrib><collection>CrossRef</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Environment Abstracts</collection><jtitle>Sheng tai xue bao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chen, Xueying</au><au>Gao, Xuejiao</au><au>Xu, Jiawei</au><au>Jin, Yinghua</au><au>Zhang, Yingjie</au><au>Wang, Cailing</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Analysis of the pattern change process of Changbai Mountain wind-damaged landscape in the past thirty years</atitle><jtitle>Sheng tai xue bao</jtitle><date>2022-08-01</date><risdate>2022</risdate><volume>42</volume><issue>4</issue><spage>1327</spage><pages>1327-</pages><issn>1000-0933</issn><abstract>The wind-damaged landscape formed by the 1986 typhoon in Changbai Mountain Nature Reserve was studied in this paper. High-definition remote sensing images in 1987, 1993, 1999, 2004, 2010 and 2016 were selected to decode to analyze the change of each patch type in the study area. Fragstats 4.2 was used to quantitatively analyze the landscape pattern indices, and a combination of principal component analysis and comprehensive landscape evaluation index was used to make a comprehensive evaluation to reveal the process of landscape pattern changes 30 years after the wind damage. The results were as follows:(1) the dominance of herbaceous-shrub kept decreasing, but the distribution was homogenous, the patch shape was regular, and the degree of aggregation was high; broad-leaved forest and coniferous forest firstly increased in large patches during the recovery process, and later on the area increase was mainly in small patches, the patch shape of broad-leaved forest tended to be regular, and coniferous forest was complex; Betula ermanii forest firstly increased in small patches, and later on the large patches grew in succession, the shape became more complicated, and there was a trend of contiguous growth.(2) At the landscape level, small and scattered patches were converted into large and concentrated patches in the restoration process, the irregularity of shape increased and the connectivity of the landscape decreased. As the restoration continues, the landscape tended to be homogenized.(3) According to the landscape transfer matrix, herbaceous-shrub patches in the study area would be continuously transformed into arboreal patches, the proportion of herbaceous-shrub gradually decreased, while arboreal increased. Among them, herbaceous-shrub mainly transformed into broad-leaved forest, broad-leaved forest mainly transformed into coniferous forest, and coniferous forest mainly transformed into Betula ermanii forest. The four patch types of herbaceous-shrub, broad-leaved forest, coniferous forest, and Betula ermanii forest showed a succession relationship during the restoration process.(4) Through the principal component analysis method, two principal components related to landscape scale and shape and landscape dispersion, respectively, were identified as key indices to characterize landscape restoration.(5) Using the combination of principal component analysis and the comprehensive landscape evaluation index to evaluate the wind-damaged landscape in Changbai Mountain, the results showed that during the 30-year restoration period, the quality of the study area was improved, but the recovery was slow and still differed significantly from that before the wind damage.(6) Multiple strong wind disturbances can form a non-standard vertical band spectrum on the western and southern slopes of Changbai Mountain.</abstract><cop>Beijing</cop><pub>Science Press</pub><doi>10.5846/stxb202101290316</doi></addata></record>
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subjects Betula ermanii
Coniferous forests
Forests
High definition
Mountains
Nature reserves
Patches (structures)
Pattern analysis
Principal components analysis
Recovery
Remote sensing
Restoration
Transfer matrices
Typhoons
Wind
Wind damage
title Analysis of the pattern change process of Changbai Mountain wind-damaged landscape in the past thirty years
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