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Title:Age-dependent moisture response of conifers near their cold range limit
Authors:ID Tumajer, Jan (Author)
ID Håkan, Grudd (Author)
ID Jevšenak, Jernej (Author)
ID Kirchhefer, Andreas J. (Author)
ID Marotta, Francesco (Author)
ID Mašek, Jiří (Author)
ID Nowatzki, Kiara Maria (Author)
ID Obojes, Nikolaus (Author)
ID Stoffel, Markus (Author)
ID Treml, V. (Author)
ID Lange, Jelena (Author)
Files:URL URL - Source URL, visit https://www.sciencedirect.com/science/article/pii/S0168192325002540?via%3Dihub
 
.pdf PDF - Presentation file, download (10,22 MB)
MD5: 1709F8AB3DF761519449D7041E017C0E
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo SciVie - Slovenian Forestry Institute
Abstract:Growth dynamics of cold subarctic and subalpine forests are primarily sensitive to temperature, but growth responses may vary across regions or shift over tree ontogeny. Systematic assessments of spatial, interspecific, and demographic variation in temperature and moisture limitation of tree growth at cold distribution margins are essential for enhancing our understanding of how these ecosystems will evolve under climate regimes. To address this gap, we built a network of 22 tree-ring width chronologies from cold forests covering two regions (Fennoscandia, European Alps), three species (Pinus sylvestris, Pinus cembra, Larix decidua), and two age cohorts (45–100 and >150 years). We combined daily climate-growth correlations with the process-based Vaganov-Shashkin growth model to identify differences in critical growth factors between species and age cohorts. In addition, we assessed the coincidence of unusually wide and narrow tree rings with years of specific climatic anomalies. Although growing season temperature was the dominant growth-limiting factor, seasonal effects of water balance on tree growth were considerably large and varied systematically between regions, species, and particularly age cohorts. The growth of young P. sylvestris in Fennoscandia responded negatively to water balance and narrow rings coincided with wet years. In contrast, the growth of young P. cembra in the Alps was drought-limited. Old trees of all species and both age cohorts of L. decidua in the Alps showed limited sensitivity to water balance. The patterns of climate-growth responses in cohort chronologies based on tree age at the year of coring were similar to ontogenetic shifts of climate-growth responses if chronologies were based on the cambial age of individual rings. Our results stress the need to account for interspecific and demographic differences in sensitivity to climate in large-scale studies of cold forest ecosystems.
Keywords:boreal forest, Larix, subalpine forest, pinus, tree ring, Vaganov-Shashkin model
Publication status:Published
Publication version:Version of Record
Publication date:01.01.2025
Year of publishing:2025
Number of pages:str. 1-13
Numbering:Vol. 371, article no. ǂ110634
PID:20.500.12556/DiRROS-22560 New window
UDC:630*5
ISSN on article:1873-2240
DOI:10.1016/j.agrformet.2025.110634 New window
COBISS.SI-ID:238278659 New window
Note:Nasl. z nasl. zaslona; Opis vira z dne 4. 6. 2025;
Publication date in DiRROS:04.06.2025
Views:546
Downloads:264
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Record is a part of a journal

Title:Agricultural and Forest Meteorology
Publisher:Elsevier
ISSN:1873-2240
COBISS.SI-ID:23059717 New window

Document is financed by a project

Funder:ARIS - Slovenian Research and Innovation Agency
Project number:P4-0107-2020
Name:Gozdna biologija, ekologija in tehnologija

Funder:EC - European Commission
Project number:871120
Name:International Network for Terrestrial Research and Monitoring in the Arctic
Acronym:INTERACT

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Secondary language

Language:Slovenian
Keywords:borealni gozdovi, macesen, bor, subalpski gozdovi, Vaganov-Šaškinov model, rastni obroč


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