Future forest distribution on Finnmarksvidda, North Norway
Finnmarksvidda is Norway's largest mountain plateau, located in the Arctic/alpineboreal transition area. The area is also a central winter grazing area for the reindeer herds of the indigenous Sámi people. This study develops a bioclimatic-based model to simulate future potential vegetation, wi...
Gespeichert in:
Veröffentlicht in: | Climate research 2017-01, Vol.73 (1 & 2), p.125-133 |
---|---|
Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
Schlagworte: | |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 133 |
---|---|
container_issue | 1 & 2 |
container_start_page | 125 |
container_title | Climate research |
container_volume | 73 |
creator | Karlsen, Stein Rune Tømmervik, Hans Johansen, Bernt Riseth, Jan Åge |
description | Finnmarksvidda is Norway's largest mountain plateau, located in the Arctic/alpineboreal transition area. The area is also a central winter grazing area for the reindeer herds of the indigenous Sámi people. This study develops a bioclimatic-based model to simulate future potential vegetation, with a focus on forest types. The model utilizes a bioclimatic study in the region, where vegetation types have been grouped according to minimum summer temperature demands. This is then used as a base for modelling of future vegetation. Due to the flat landscape of Finnmarksvidda, the model shows that a 1°C increase in summer temperatures will potentially lead to an increase of forested areas by 4485 km², which is a 70% increase from the current 6900 km² to a simulated 11 706 km². This in turn will lead to a reduction of Arctic-alpine heaths from 4440 km² today to potentially only 670 km². Such changes will have consequences for the reindeer grazing system, as the predicted changes will lead to a decrease in the vegetation types that have high winter grazing accessibility for reindeer, from 2386 km² today to potentially only 377 km². On the other hand, vegetation types with medium accessibility will experience an increase, from 2857 to 3366 km². |
doi_str_mv | 10.3354/cr01459 |
format | Article |
fullrecord | <record><control><sourceid>jstor_proqu</sourceid><recordid>TN_cdi_proquest_journals_2002180381</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><jstor_id>26394431</jstor_id><sourcerecordid>26394431</sourcerecordid><originalsourceid>FETCH-LOGICAL-c308t-3ec4a6c870cd11ab794cb37091262f0ce4f83ba2b99cd90d06a7c5950cd42e2a3</originalsourceid><addsrcrecordid>eNo9kE1LxDAQhoMoWFfxFwgFD16sTj6aNN5ksSoselHwFtI0xVZt1iRV9t-bpYswzFwe5v1A6BTDFaUluzYeMCvlHsowx7zApSD7KANJeVEK8XaIjkIYAIBUAjJ0U09x8jbvnLch5m0fou-bKfZuzNPU_Th-af8Rfvq21Zf5k_Pxfbt_9eYYHXT6M9iT3V2g1_ruZflQrJ7vH5e3q8JQqGJBrWGam6RmWox1IyQzDRUgMeGkA2NZV9FGk0ZK00pogWthSlkmnBFLNF2g8_nv2rvvKblUg5v8mCQVSTFwBbTCibqYKeNdCN52au37ZH2jMKhtMWpXTCLPZnII0fl_jHAqGaOY_gH5r16Z</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2002180381</pqid></control><display><type>article</type><title>Future forest distribution on Finnmarksvidda, North Norway</title><source>Inter-Research</source><source>JSTOR Archive Collection A-Z Listing</source><source>Alma/SFX Local Collection</source><creator>Karlsen, Stein Rune ; Tømmervik, Hans ; Johansen, Bernt ; Riseth, Jan Åge</creator><creatorcontrib>Karlsen, Stein Rune ; Tømmervik, Hans ; Johansen, Bernt ; Riseth, Jan Åge</creatorcontrib><description>Finnmarksvidda is Norway's largest mountain plateau, located in the Arctic/alpineboreal transition area. The area is also a central winter grazing area for the reindeer herds of the indigenous Sámi people. This study develops a bioclimatic-based model to simulate future potential vegetation, with a focus on forest types. The model utilizes a bioclimatic study in the region, where vegetation types have been grouped according to minimum summer temperature demands. This is then used as a base for modelling of future vegetation. Due to the flat landscape of Finnmarksvidda, the model shows that a 1°C increase in summer temperatures will potentially lead to an increase of forested areas by 4485 km², which is a 70% increase from the current 6900 km² to a simulated 11 706 km². This in turn will lead to a reduction of Arctic-alpine heaths from 4440 km² today to potentially only 670 km². Such changes will have consequences for the reindeer grazing system, as the predicted changes will lead to a decrease in the vegetation types that have high winter grazing accessibility for reindeer, from 2386 km² today to potentially only 377 km². On the other hand, vegetation types with medium accessibility will experience an increase, from 2857 to 3366 km².</description><identifier>ISSN: 0936-577X</identifier><identifier>EISSN: 1616-1572</identifier><identifier>DOI: 10.3354/cr01459</identifier><language>eng</language><publisher>Oldendorf: Inter-Research</publisher><subject>Accessibility ; Alpine environments ; Area ; Bioclimatology ; Biometeorology ; Computer simulation ; Forests ; Grazing ; Heaths ; Landscape ; Modelling ; Plateaus ; Polar environments ; Reindeer ; Summer ; Summer temperatures ; Vegetation ; Winter</subject><ispartof>Climate research, 2017-01, Vol.73 (1 & 2), p.125-133</ispartof><rights>The author 2017</rights><rights>Copyright Inter-Research Science Center 2017</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c308t-3ec4a6c870cd11ab794cb37091262f0ce4f83ba2b99cd90d06a7c5950cd42e2a3</citedby><cites>FETCH-LOGICAL-c308t-3ec4a6c870cd11ab794cb37091262f0ce4f83ba2b99cd90d06a7c5950cd42e2a3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/26394431$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/26394431$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,3759,27924,27925,58017,58250</link.rule.ids></links><search><creatorcontrib>Karlsen, Stein Rune</creatorcontrib><creatorcontrib>Tømmervik, Hans</creatorcontrib><creatorcontrib>Johansen, Bernt</creatorcontrib><creatorcontrib>Riseth, Jan Åge</creatorcontrib><title>Future forest distribution on Finnmarksvidda, North Norway</title><title>Climate research</title><description>Finnmarksvidda is Norway's largest mountain plateau, located in the Arctic/alpineboreal transition area. The area is also a central winter grazing area for the reindeer herds of the indigenous Sámi people. This study develops a bioclimatic-based model to simulate future potential vegetation, with a focus on forest types. The model utilizes a bioclimatic study in the region, where vegetation types have been grouped according to minimum summer temperature demands. This is then used as a base for modelling of future vegetation. Due to the flat landscape of Finnmarksvidda, the model shows that a 1°C increase in summer temperatures will potentially lead to an increase of forested areas by 4485 km², which is a 70% increase from the current 6900 km² to a simulated 11 706 km². This in turn will lead to a reduction of Arctic-alpine heaths from 4440 km² today to potentially only 670 km². Such changes will have consequences for the reindeer grazing system, as the predicted changes will lead to a decrease in the vegetation types that have high winter grazing accessibility for reindeer, from 2386 km² today to potentially only 377 km². On the other hand, vegetation types with medium accessibility will experience an increase, from 2857 to 3366 km².</description><subject>Accessibility</subject><subject>Alpine environments</subject><subject>Area</subject><subject>Bioclimatology</subject><subject>Biometeorology</subject><subject>Computer simulation</subject><subject>Forests</subject><subject>Grazing</subject><subject>Heaths</subject><subject>Landscape</subject><subject>Modelling</subject><subject>Plateaus</subject><subject>Polar environments</subject><subject>Reindeer</subject><subject>Summer</subject><subject>Summer temperatures</subject><subject>Vegetation</subject><subject>Winter</subject><issn>0936-577X</issn><issn>1616-1572</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNo9kE1LxDAQhoMoWFfxFwgFD16sTj6aNN5ksSoselHwFtI0xVZt1iRV9t-bpYswzFwe5v1A6BTDFaUluzYeMCvlHsowx7zApSD7KANJeVEK8XaIjkIYAIBUAjJ0U09x8jbvnLch5m0fou-bKfZuzNPU_Th-af8Rfvq21Zf5k_Pxfbt_9eYYHXT6M9iT3V2g1_ruZflQrJ7vH5e3q8JQqGJBrWGam6RmWox1IyQzDRUgMeGkA2NZV9FGk0ZK00pogWthSlkmnBFLNF2g8_nv2rvvKblUg5v8mCQVSTFwBbTCibqYKeNdCN52au37ZH2jMKhtMWpXTCLPZnII0fl_jHAqGaOY_gH5r16Z</recordid><startdate>20170101</startdate><enddate>20170101</enddate><creator>Karlsen, Stein Rune</creator><creator>Tømmervik, Hans</creator><creator>Johansen, Bernt</creator><creator>Riseth, Jan Åge</creator><general>Inter-Research</general><general>Inter-Research Science Center</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>7TN</scope><scope>C1K</scope><scope>F1W</scope><scope>KL.</scope><scope>SOI</scope></search><sort><creationdate>20170101</creationdate><title>Future forest distribution on Finnmarksvidda, North Norway</title><author>Karlsen, Stein Rune ; Tømmervik, Hans ; Johansen, Bernt ; Riseth, Jan Åge</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c308t-3ec4a6c870cd11ab794cb37091262f0ce4f83ba2b99cd90d06a7c5950cd42e2a3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Accessibility</topic><topic>Alpine environments</topic><topic>Area</topic><topic>Bioclimatology</topic><topic>Biometeorology</topic><topic>Computer simulation</topic><topic>Forests</topic><topic>Grazing</topic><topic>Heaths</topic><topic>Landscape</topic><topic>Modelling</topic><topic>Plateaus</topic><topic>Polar environments</topic><topic>Reindeer</topic><topic>Summer</topic><topic>Summer temperatures</topic><topic>Vegetation</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Karlsen, Stein Rune</creatorcontrib><creatorcontrib>Tømmervik, Hans</creatorcontrib><creatorcontrib>Johansen, Bernt</creatorcontrib><creatorcontrib>Riseth, Jan Åge</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Environment Abstracts</collection><jtitle>Climate research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Karlsen, Stein Rune</au><au>Tømmervik, Hans</au><au>Johansen, Bernt</au><au>Riseth, Jan Åge</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Future forest distribution on Finnmarksvidda, North Norway</atitle><jtitle>Climate research</jtitle><date>2017-01-01</date><risdate>2017</risdate><volume>73</volume><issue>1 & 2</issue><spage>125</spage><epage>133</epage><pages>125-133</pages><issn>0936-577X</issn><eissn>1616-1572</eissn><abstract>Finnmarksvidda is Norway's largest mountain plateau, located in the Arctic/alpineboreal transition area. The area is also a central winter grazing area for the reindeer herds of the indigenous Sámi people. This study develops a bioclimatic-based model to simulate future potential vegetation, with a focus on forest types. The model utilizes a bioclimatic study in the region, where vegetation types have been grouped according to minimum summer temperature demands. This is then used as a base for modelling of future vegetation. Due to the flat landscape of Finnmarksvidda, the model shows that a 1°C increase in summer temperatures will potentially lead to an increase of forested areas by 4485 km², which is a 70% increase from the current 6900 km² to a simulated 11 706 km². This in turn will lead to a reduction of Arctic-alpine heaths from 4440 km² today to potentially only 670 km². Such changes will have consequences for the reindeer grazing system, as the predicted changes will lead to a decrease in the vegetation types that have high winter grazing accessibility for reindeer, from 2386 km² today to potentially only 377 km². On the other hand, vegetation types with medium accessibility will experience an increase, from 2857 to 3366 km².</abstract><cop>Oldendorf</cop><pub>Inter-Research</pub><doi>10.3354/cr01459</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0936-577X |
ispartof | Climate research, 2017-01, Vol.73 (1 & 2), p.125-133 |
issn | 0936-577X 1616-1572 |
language | eng |
recordid | cdi_proquest_journals_2002180381 |
source | Inter-Research; JSTOR Archive Collection A-Z Listing; Alma/SFX Local Collection |
subjects | Accessibility Alpine environments Area Bioclimatology Biometeorology Computer simulation Forests Grazing Heaths Landscape Modelling Plateaus Polar environments Reindeer Summer Summer temperatures Vegetation Winter |
title | Future forest distribution on Finnmarksvidda, North Norway |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T23%3A51%3A57IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-jstor_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Future%20forest%20distribution%20on%20Finnmarksvidda,%20North%20Norway&rft.jtitle=Climate%20research&rft.au=Karlsen,%20Stein%20Rune&rft.date=2017-01-01&rft.volume=73&rft.issue=1%20&%202&rft.spage=125&rft.epage=133&rft.pages=125-133&rft.issn=0936-577X&rft.eissn=1616-1572&rft_id=info:doi/10.3354/cr01459&rft_dat=%3Cjstor_proqu%3E26394431%3C/jstor_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=2002180381&rft_id=info:pmid/&rft_jstor_id=26394431&rfr_iscdi=true |