Effects of Climate Change on Tree-Ring Growth

A special issue of Forests (ISSN 1999-4907). This special issue belongs to the section "Forest Ecology and Management".

Deadline for manuscript submissions: 29 August 2024 | Viewed by 2378

Special Issue Editors


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Guest Editor
College of Forestry, Hebei Agricultural University, Baoding 071001, China
Interests: climate modeling; tree-ring analysis; tree growth; climate dynamics; climatology

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Guest Editor
Institute of Geographic Resources and Environment, Chinese Academy of Sciences, Beijing 100101, China
Interests: ecosystem ecology; forest ecology; climate change

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Guest Editor
College of Biology and the Environment, Nanjing Forestry University, Nanjing 210037, China
Interests: treeline ecotone; dendroecology; alpine shrub; climate warming; Tibetan Plateau
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Guest Editor
Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an 710049, China
Interests: tree-ring isotopes; climate change; climate reconstruction
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Special Issue Information

Dear Colleagues,

Forest dynamics have shown pervasive shifts in a changing world. Climate change can cause tree growth decline and high tree mortality across global forests. Tree-ring growth response to climate change determines whether tree species have high tree mortality in this changing world. We would like to invite contributions on the effects of climate change on tree-ring growth. Contributions to this Special Issue are invited that explore all aspects of tree-ring studies that are related to:

  • Forest carbon dynamics and climate change;
  • Climate-change-induced tree-line movement, insect outbreaks, or forest dynamics with tree rings;
  • Response and adaptation of tree or shrub growth to climate change;
  • Tree-ring based past climate reconstruction;
  • Wood anatomy of tree rings, tree growth monitoring, and climate change;
  • Fusing tree‐ring and forest inventory data
  • Linking remote sensing and dendrochronology

Prof. Dr. Xianliang Zhang
Dr. Liang Shi
Dr. Yafeng Wang
Prof. Dr. Qiang Li
Guest Editors

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Keywords

  • tree-ring
  • dendroecology
  • stable isotopes
  • extreme climate events
  • drought
  • forest growth
  • climate changes

Published Papers (2 papers)

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Research

13 pages, 3232 KiB  
Article
Solar and Climatic Factors Affecting Tree-Ring Growth of Mountain Birch (Betula pubescens) beyond the Northern Timberline on Kola Peninsula, Northwestern Russia
by Oleg I. Shumilov, Elena A. Kasatkina and Evgeniy O. Potorochin
Forests 2024, 15(1), 37; https://doi.org/10.3390/f15010037 - 23 Dec 2023
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Abstract
A 105-year chronology (AD 1917–2021) was developed from mountain birch (Betula pubescens Ehrh.) from beyond the coniferous treeline on the Kola Peninsula in Northwestern Russia (68.86 N, 34.69 E). A total of 22 trees were cored, including the oldest living mountain birch [...] Read more.
A 105-year chronology (AD 1917–2021) was developed from mountain birch (Betula pubescens Ehrh.) from beyond the coniferous treeline on the Kola Peninsula in Northwestern Russia (68.86 N, 34.69 E). A total of 22 trees were cored, including the oldest living mountain birch of 105 years old. The highest correlations occurred for the May temperature (r = 0.39, p < 0.01) and July sunshine duration (r = −0.39, p < 0.05). The increase in radial growth in May seemed to be caused by snowmelt giving rise to soil temperature, which can lead to a resumption in radial growth after winter dormancy. The negative correlation with the July sunshine duration seemed to be connected to changes in the spectral composition of solar radiation in the red to far-red ratio in the end of the polar day in July. The application of wavelet coherency revealed a significant (>95%) connection between the radial growth of B. pubescens, and solar activity in frequency bands encompassed the main solar cycles: 5.5 years (the second harmonic of the Schwabe cycle), 11 years (the Schwabe cycle) and 22 years (the Hale cycle). The results show that the northernmost birch trees in Europe are suited for tree-ring research. This allows us to expand the area of dendrochronological research further beyond the conifer treeline above the Polar Circle. Full article
(This article belongs to the Special Issue Effects of Climate Change on Tree-Ring Growth)
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14 pages, 3116 KiB  
Article
Radial Growth–Climate Relationship Varies with Spatial Distribution of Schima superba Stands in Southeast China’s Subtropical Forests
by Shaowei Jiang, Xiali Guo, Ping Zhao and Hanxue Liang
Forests 2023, 14(7), 1291; https://doi.org/10.3390/f14071291 - 22 Jun 2023
Cited by 2 | Viewed by 1129
Abstract
To understand the impact of climate change on the tree radial growth in Southeast China’s subtropical evergreen broadleaved forest, comparative research on the radial growth–climate associations of Schima superba was conducted. This dominant evergreen broadleaved tree species was examined at both its southern [...] Read more.
To understand the impact of climate change on the tree radial growth in Southeast China’s subtropical evergreen broadleaved forest, comparative research on the radial growth–climate associations of Schima superba was conducted. This dominant evergreen broadleaved tree species was examined at both its southern and northern distribution margins through dendroclimatology. The results showed that the radial growth of S. superba stands at a high elevation in the southern margin and stands in the northern margin were positively correlated with springtime temperatures, mostly in April (e.g., mean temperature: r = 0.630, p < 0.05) and May (e.g., maximum temperature: r = 0.335, p < 0.05), respectively. Meanwhile, the temperature in the late rainy season had a significant negative effect on the radial growth of S. superba stands in the southern margin, including high-elevation stands (e.g., the mean temperature in previous and current September: r = −0.437 and −0.383, p < 0.05) and low-elevation stands (e.g., the mean temperature in previous August and October: r = −0.577 and −0.348, p < 0.05). It was shown that temperature was the key climatic factor affecting the radial growth of S. superba, and the response of radial growth to temperature had obvious spatial differences. The findings indicate that the radial growth of S. superba stands in warm growth environments will be negatively impacted by future climate warming. On the contrary, the radial growth of S. superba stands growing in relatively cold growth environments may benefit from warmer spring. The results enhance the understanding of tree growth responses to climate change in the subtropical forests of China. Full article
(This article belongs to the Special Issue Effects of Climate Change on Tree-Ring Growth)
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