Literature DB >> 31860143

Tree growth influenced by warming winter climate and summer moisture availability in northern temperate forests.

Jill E Harvey1,2, Marko Smiljanić1, Tobias Scharnweber1, Allan Buras3, Anna Cedro4, Roberto Cruz-García1, Igor Drobyshev5,6, Karolina Janecka1, Āris Jansons7, Ryszard Kaczka8, Marcin Klisz9, Alar Läänelaid10, Roberts Matisons7, Lena Muffler1,11, Kristina Sohar10, Barbara Spyt8, Juliane Stolz12, Ernst van der Maaten12, Marieke van der Maaten-Theunissen12, Adomas Vitas13, Robert Weigel1,11, Jürgen Kreyling1, Martin Wilmking1.   

Abstract

The role of future forests in global biogeochemical cycles will depend on how different tree species respond to climate. Interpreting the response of forest growth to climate change requires an understanding of the temporal and spatial patterns of seasonal climatic influences on the growth of common tree species. We constructed a new network of 310 tree-ring width chronologies from three common tree species (Quercus robur, Pinus sylvestris and Fagus sylvatica) collected for different ecological, management and climate purposes in the south Baltic Sea region at the border of three bioclimatic zones (temperate continental, oceanic, southern boreal). The major climate factors (temperature, precipitation, drought) affecting tree growth at monthly and seasonal scales were identified. Our analysis documents that 20th century Scots pine and deciduous species growth is generally controlled by different climate parameters, and that summer moisture availability is increasingly important for the growth of deciduous species examined. We report changes in the influence of winter climate variables over the last decades, where a decreasing influence of late winter temperature on deciduous tree growth and an increasing influence of winter temperature on Scots pine growth was found. By comparing climate-growth responses for the 1943-1972 and 1973-2002 periods and characterizing site-level growth response stability, a descriptive application of spatial segregation analysis distinguished sites with stable responses to dominant climate parameters (northeast of the study region), and sites that collectively showed unstable responses to winter climate (southeast of the study region). The findings presented here highlight the temporally unstable and nonuniform responses of tree growth to climate variability, and that there are geographical coherent regions where these changes are similar. Considering continued climate change in the future, our results provide important regional perspectives on recent broad-scale climate-growth relationships for trees across the temperate to boreal forest transition around the south Baltic Sea.
© 2019 The Authors. Global Change Biology published by John Wiley & Sons Ltd.

Entities:  

Keywords:  Baltic Sea; Europe; climate change; climate-growth relationships; dendroecology; tree growth; tree-ring network; winter climate

Year:  2019        PMID: 31860143     DOI: 10.1111/gcb.14966

Source DB:  PubMed          Journal:  Glob Chang Biol        ISSN: 1354-1013            Impact factor:   10.863


  4 in total

1.  Radial Growth of Trees Rather Than Shrubs in Boreal Forests Is Inhibited by Drought.

Authors:  Jingwen Yang; Qiuliang Zhang; Wenqi Song; Xu Zhang; Xiaochun Wang
Journal:  Front Plant Sci       Date:  2022-06-02       Impact factor: 6.627

2.  Low-Altitude Boundary of Abies faxoniana Is More Susceptible to Long-Term Open-Top Chamber Warming in the Eastern Tibetan Plateau.

Authors:  Haifeng Song; Qingquan Han; Sheng Zhang
Journal:  Front Plant Sci       Date:  2021-12-03       Impact factor: 5.753

3.  Warming-induced drought leads to tree growth decline in subtropics: Evidence from tree rings in central China.

Authors:  Mengdan Jing; Liangjun Zhu; Shuguang Liu; Yang Cao; Yu Zhu; Wende Yan
Journal:  Front Plant Sci       Date:  2022-09-23       Impact factor: 6.627

4.  Determining the role of climate change in India's past forest loss.

Authors:  Alice E Haughan; Nathalie Pettorelli; Simon G Potts; Deepa Senapathi
Journal:  Glob Chang Biol       Date:  2022-03-23       Impact factor: 13.211

  4 in total

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