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dc.contributor.authorFomin, V.en
dc.contributor.authorMikhailovich, A.en
dc.contributor.authorGolikov, D.en
dc.contributor.authorAgapitov, E.en
dc.date.accessioned2022-10-19T05:19:23Z-
dc.date.available2022-10-19T05:19:23Z-
dc.date.issued2022-
dc.identifier.citationReconstruction of the Expansion of Siberian Larch into the Mountain Tundra in the Polar Urals in the 20th—Early 21st Centuries / V. Fomin, A. Mikhailovich, D. Golikov et al. // Forests. — 2022. — Vol. 13. — Iss. 3. — 419.en
dc.identifier.issn19994907-
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85126608685&doi=10.3390%2ff13030419&partnerID=40&md5=bf01c980b88eddfff10255f8ebafdf21link
dc.identifier.urihttp://elar.urfu.ru/handle/10995/117789-
dc.description.abstractThis paper presents results of analyzing the second half of the 20th–early 21st century changes in lateral spatial structure of Larix sibirica Ledeb. population in the upper treeline ecotone located on the Rai-Iz massif (Polar Urals, Russia). The GIS layers characterizing distribution of Siberian larch trees and undergrowth together with their crowns was produced for a 7.32 square kilometer area based on aerial images recognition. Using statistical models, we assessed probabilities for assigning trees to age intervals of 1–10, 11–40, and 40+ years based on the average radius of tree crown projection. These maps and layer showing locations of trees that grew in the upper part of the ecotone, and died during the Little Ice Age, allow for assessing specifics of forest cover proliferation at different parts of upper treeline ecotone, and comparing current location of the trees with one from the past. The proposed method for probability-based recognition of Siberian larch tree generations in the upper treeline ecotone using average crown radius can be used to reconstruct time and spatial forest dynamics at the upper growth boundaries for time spans up to 100 years and more. © 2022 by the authors. Licensee MDPI, Basel, Switzerland.en
dc.description.sponsorshipFEUG-2020-0013, FEUG-2021-0009en
dc.description.sponsorshipFunding: This research was collaboratively funded by the Russian Ministry for Science and Education (projects No. FEUG-2020-0013, No. FEUG-2021-0009). An approach to the selection of generations of trees by crown diameter was developed within the framework of the project of the Russian Ministry for Science and Education No. FEUZ-2021-0014.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherMDPIen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.sourceForestsen
dc.subjectLARIX SIBIRICA LEDEBen
dc.subjectPOLAR URALSen
dc.subjectTREELINE ECOTONEen
dc.subjectTREESen
dc.subjectUPWARD SHIFTen
dc.subjectANTENNASen
dc.subjectGIS LAYERSen
dc.subjectLARCH-TREEen
dc.subjectLARIX SIBIRICAen
dc.subjectLARIX SIBIRICA LEDEBen
dc.subjectPOLAR URALSen
dc.subjectSPATIAL STRUCTUREen
dc.subjectTREEen
dc.subjectTREELINEen
dc.subjectTREELINE ECOTONEen
dc.subjectUPWARD SHIFTen
dc.subjectFORESTRYen
dc.subjectCANOPY ARCHITECTUREen
dc.subjectCONIFEROUS TREEen
dc.subjectDECIDUOUS TREEen
dc.subjectECOTONEen
dc.subjectFOREST COVERen
dc.subjectGISen
dc.subjectMOUNTAIN REGIONen
dc.subjectPOPULATION DISTRIBUTIONen
dc.subjectPOPULATION DYNAMICSen
dc.subjectPOPULATION GROWTHen
dc.subjectPOPULATION STRUCTUREen
dc.subjectRANGE EXPANSIONen
dc.subjectRECONSTRUCTIONen
dc.subjectTEMPORAL VARIATIONen
dc.subjectTREELINEen
dc.subjectTUNDRAen
dc.subjectTWENTIETH CENTURYen
dc.subjectTWENTY FIRST CENTURYen
dc.subjectFORESTRYen
dc.subjectIMAGESen
dc.subjectLARIX SIBIRICAen
dc.subjectPROBABILITYen
dc.subjectRADIUSen
dc.subjectRUSSIAN FEDERATIONen
dc.subjectURALSen
dc.titleReconstruction of the Expansion of Siberian Larch into the Mountain Tundra in the Polar Urals in the 20th—Early 21st Centuriesen
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.typeinfo:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.3390/f13030419-
dc.identifier.scopus85126608685-
local.contributor.employeeFomin, V., Institute of Forest and Natural Resource Management, Ural State Forest Engineering University, Sibirskiy Trakt, 37, Yekaterinburg, 620100, Russian Federation, Institute of Natural Sciences and Mathematics, Ural Federal University, 19 Mira Street, Yekaterinburg, 620002, Russian Federationen
local.contributor.employeeMikhailovich, A., Institute of Physics and Technology, Ural Federal University, 19 Mira Street, Yekaterinburg, 620002, Russian Federationen
local.contributor.employeeGolikov, D., Botanic Garden of the Ural Branch of Russian Academy of Sciences, 8 Marta Street, 202a, Yekaterinburg, 620144, Russian Federationen
local.contributor.employeeAgapitov, E., Institute of Forest and Natural Resource Management, Ural State Forest Engineering University, Sibirskiy Trakt, 37, Yekaterinburg, 620100, Russian Federationen
local.issue3-
local.volume13-
dc.identifier.wos000776903100001-
local.contributor.departmentInstitute of Forest and Natural Resource Management, Ural State Forest Engineering University, Sibirskiy Trakt, 37, Yekaterinburg, 620100, Russian Federationen
local.contributor.departmentInstitute of Natural Sciences and Mathematics, Ural Federal University, 19 Mira Street, Yekaterinburg, 620002, Russian Federationen
local.contributor.departmentInstitute of Physics and Technology, Ural Federal University, 19 Mira Street, Yekaterinburg, 620002, Russian Federationen
local.contributor.departmentBotanic Garden of the Ural Branch of Russian Academy of Sciences, 8 Marta Street, 202a, Yekaterinburg, 620144, Russian Federationen
local.identifier.pure29828439-
local.description.order419-
local.identifier.eid2-s2.0-85126608685-
local.identifier.wosWOS:000776903100001-
local.fund.feuzFEUG-2020-0013-
local.fund.feuzFEUG-2021-0009-
local.fund.feuzFEUZ-2021-0014-
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