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Growth responses of Norway spruce to weather variation across Finland over the past 60 years

dc.contributor.authorLee, Daesung
dc.contributor.authorHaakana, Helena
dc.contributor.authorTikkasalo, Olli-Pekka
dc.contributor.authorMäkinen, Harri
dc.contributor.departmentid4100110310
dc.contributor.departmentid4100310510
dc.contributor.departmentid4100310610
dc.contributor.departmentid4100110310
dc.contributor.orcidhttps://orcid.org/0000-0003-1586-9385
dc.contributor.orcidhttps://orcid.org/0000-0002-4830-800X
dc.contributor.orcidhttps://orcid.org/0000-0003-1729-6349
dc.contributor.orcidhttps://orcid.org/0000-0002-1820-6264
dc.contributor.organizationLuonnonvarakeskus
dc.date.accessioned2026-06-08T14:03:57Z
dc.date.issued2026
dc.description.abstractTo understand the effects of climate change on boreal forest productivity, it is crucial to examine tree growth variation and identify the climatic factors impacting it. Norway spruce (Picea abies (L.) Karst.) is a common and economically important tree species in Northern and Central Europe. Despite being sensitive to drought, it has been the preferred species for regeneration. Using an extensive tree-ring dataset collected as part of the Finnish National Forest Inventory, we identified the primary weather factors affecting annual radial growth variation in 4979 individual trees over the 1961–2023. We also analysed the spatial patterns of these relationships across Finland. This large-scale analysis revealed that high June temperatures promote tree growth at northern latitudes while the growth response to precipitation is weak. A clear south-north trend was observed in the weather-growth relationships. In southern and central Finland, warm, dry summers were detrimental to spruce growth. However, high June temperatures the previous year were negatively related to radial growth across the country. Furthermore, radial growth negatively responded to high winter temperatures. These results imply that temperature-induced water stress already limits spruce growth more severely and over a larger region than expected. It is likely that the anticipated benefits of global warming due to higher temperatures are diminished or negated by lower soil moisture availability or increased atmospheric evaporative demand.
dc.format.pagerange11 p.
dc.identifier.citationHow to cite: Daesung Lee, Helena Haakana, Olli-Pekka Tikkasalo, Harri Mäkinen, Growth responses of Norway spruce to weather variation across Finland over the past 60 years, Forest Ecology and Management, Volume 618, 2026, 123967, ISSN 0378-1127, https://doi.org/10.1016/j.foreco.2026.123967
dc.identifier.urihttps://jukuri.luke.fi/handle/11111/104101
dc.identifier.urlhttps://doi.org/10.1016/j.foreco.2026.123967
dc.identifier.urnURN:NBN:fi-fe2026060865113
dc.language.isoen
dc.okm.avoinsaatavuuskytkin1 = Avoimesti saatavilla
dc.okm.corporatecopublicationei
dc.okm.discipline4112
dc.okm.internationalcopublicationei
dc.okm.julkaisukanavaoa2 = Osittain avoimessa julkaisukanavassa ilmestynyt julkaisu
dc.okm.selfarchivedon
dc.publisherElsevier
dc.relation.articlenumber123967
dc.relation.doi10.1016/j.foreco.2026.123967
dc.relation.ispartofseriesForest ecology and management
dc.relation.issn0378-1127
dc.relation.issn1872-7042
dc.relation.volume618
dc.rightsCC BY 4.0
dc.source.justusid141794
dc.subjectboreal forests
dc.subjectclimate change
dc.subjectdendroecology
dc.subjectPicea abies (L.) Karst.
dc.subjectradial increment
dc.teh41007-00305900
dc.teh41007-00270401
dc.teh41007-00333101
dc.titleGrowth responses of Norway spruce to weather variation across Finland over the past 60 years
dc.typepublication
dc.type.okmfi=A1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä|sv=A1 Originalartikel i en vetenskaplig tidskrift|en=A1 Journal article (refereed), original research|
dc.type.versionfi=Publisher's version|sv=Publisher's version|en=Publisher's version|

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