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dc.contributor.authorFomin, V. V.en
dc.contributor.authorMikhailovich, A. P.en
dc.contributor.authorShiyatov, S. G.en
dc.date.accessioned2021-08-31T15:01:46Z-
dc.date.available2021-08-31T15:01:46Z-
dc.date.issued2020-
dc.identifier.citationFomin V. V. Trees in the Upper Treeline Ecotone in the Polar Urals: Centuries-Old Change and Spatial Patterns / V. V. Fomin, A. P. Mikhailovich, S. G. Shiyatov. — DOI 10.1659/MRD-JOURNAL-D-20-00002.1 // Mountain Research and Development. — 2020. — Vol. 40. — Iss. 2. — P. R32-R40.en
dc.identifier.issn2764741-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Gold3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85100934813&doi=10.1659%2fMRD-JOURNAL-D-20-00002.1&partnerID=40&md5=6234c3cece1f390822b4fb4688faee65
dc.identifier.urihttp://elar.urfu.ru/handle/10995/102095-
dc.description.abstractWoody vegetation at the upper limit of its growth is a sensitive indicator of climate change. The aim of this study is to provide an analysis of the centuries-old spatiotemporal dynamics of larch trees at the upper limit of their growth (mountain massif Rai-Iz, Polar Urals, Russia). We used a ground-based method of mapping the remnants of trees that grew in the study area and died during the Little Ice Age. Aerial photographs from the 1960s and high-spatial-resolution satellite images from 2015 were used as data sources to define the locations of trees. Maps of the forest-Tundra phytocoenochoras (areas of the terrain that are relatively homogeneous for one or more components of vegetation and/or other indicators) were created using a modified method of boundary detection between forest parcels with different stand densities. The proposed method of boundary detection between the main types of phytocoenochoras allowed us to identify a 15% total increase in areas of closed and open forest and areas with sparse tree growth, as well as a decrease in areas of tundra with single trees over these last decades. Using our spatiotemporal analysis of forest-Tundra demographics over the last 50 years, we found that the number of trees in the ecotone had doubled. However, modern trees have not yet reached the areas occupied by trees in the past. ©en
dc.description.sponsorshipThis work was supported by the Russian Foundation for Basic Research (project 18-34-00803 mol_a). Some studies related to the assessment of the spatial distribution of snow at the beginning of the growing season were carried out within a grant from the Russian Science Foundation (project 17-14-01112) and a grant from the Russian Ministry for Education and Science (FEUG-2020-0013). We express our gratitude to Dmitriy Golikov and Yegor Agapitov for their help in setting up forest plots and data processing, and also to Denis Kapralov for help in mapping the tree remnants.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherInternational Mountain Societyen
dc.relationinfo:eu-repo/grantAgreement/RSF//17-14-01112en
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceMt. Res. Dev.2
dc.sourceMountain Research and Developmenten
dc.subjectBOUNDARY DETECTIONen
dc.subjectCLIMATE-DRIVEN SHIFTen
dc.subjectPOLAR URALSen
dc.subjectSPATIOTEMPORAL DYNAMICSen
dc.subjectUPPER TREELINE ECOTONEen
dc.subjectDECIDUOUS TREEen
dc.subjectDETECTION METHODen
dc.subjectECOTONEen
dc.subjectSPATIOTEMPORAL ANALYSISen
dc.subjectTREELINEen
dc.subjectURALSen
dc.subjectINDICATOR INDICATORen
dc.titleTrees in the Upper Treeline Ecotone in the Polar Urals: Centuries-Old Change and Spatial Patternsen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.1659/MRD-JOURNAL-D-20-00002.1-
dc.identifier.scopus85100934813-
local.contributor.employeeFomin, V.V., GIS-Technologies Research Laboratory in Ecology and Forest Sciences, Ural State Forest Engineering University, Sibirskiy Trakt 37, Yekaterinburg, 620100, Russian Federation, Laboratory of Dendrochronology, Institute of Plant and Animal Ecology, 8 Marta Street 202, Yekaterinburg, 620144, Russian Federation
local.contributor.employeeMikhailovich, A.P., Department of Physical Methods and Devices for Quality Control, Ural Federal University, Mira Street 19, Yekaterinburg, 620002, Russian Federation
local.contributor.employeeShiyatov, S.G., Laboratory of Dendrochronology, Institute of Plant and Animal Ecology, 8 Marta Street 202, Yekaterinburg, 620144, Russian Federation
local.description.firstpageR32-
local.description.lastpageR40-
local.issue2-
local.volume40-
dc.identifier.wos000620442000014-
local.contributor.departmentGIS-Technologies Research Laboratory in Ecology and Forest Sciences, Ural State Forest Engineering University, Sibirskiy Trakt 37, Yekaterinburg, 620100, Russian Federation
local.contributor.departmentLaboratory of Dendrochronology, Institute of Plant and Animal Ecology, 8 Marta Street 202, Yekaterinburg, 620144, Russian Federation
local.contributor.departmentDepartment of Physical Methods and Devices for Quality Control, Ural Federal University, Mira Street 19, Yekaterinburg, 620002, Russian Federation
local.identifier.pure6ebad9b3-6f8f-4232-b328-c983aaa1c24euuid
local.identifier.pure21024460-
local.identifier.eid2-s2.0-85100934813-
local.fund.rsf17-14-01112-
local.fund.rffi18-34-00803-
local.identifier.wosWOS:000620442000014-
local.fund.feuzFEUG-2020-0013-
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