Tree-Ring Analysis: Response and Adaptation to Climate Change

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

Deadline for manuscript submissions: closed (31 December 2025) | Viewed by 2270

Special Issue Editors


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Guest Editor
Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias, CENID-RASPA, Gomez Palacio 35150, Mexico
Interests: climate reconstruction; analysis by machine learning; spatial analysis of tree-ring; remote sensing; machine learning; biogeography; climate change

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Guest Editor
Instituto Nacional de Investigaciones Forestales, Agrícolas y Pecuarias, CENID-RASPA, Gomez Palacio 35150, Mexico
Interests: paleoclimatology; drought reconstruction; tree-ring research; climate change tree-ring; ENSO; monsoon; climate

Special Issue Information

Dear Colleagues,

The analysis of tree rings, or dendrochronology, is a fundamental tool for understanding the impacts of climate change on forest ecosystems. One of the most significant areas in this field is the reconstruction of historical climates, as growth rings provide valuable information about past environmental conditions, such as temperature and precipitation, allowing scientists to identify patterns of change over time. Additionally, this analysis helps with the assessment of different tree species’ resilience and ability to adapt to adverse climatic conditions, which is crucial for biodiversity conservation. Research in this area is also related to the carbon cycle, as tree growth influences carbon storage in ecosystems, a key factor in combating climate change. Another important aspect is phenology, the study of growth and reproduction cycles in trees, which can reveal how they are responding to variations in temperature and water availability. Finally, the data obtained can guide sustainable forest management practices and habitat restoration projects, helping to mitigate the effects of climate change and promote the resilience of forest ecosystems. Together, these areas offer a comprehensive understanding of how climate change affects forests and enable the development of effective strategies for their conservation and management. This Special Issue aims to compile scientific articles on tree ring analysis and climate change. It will include manuscripts addressing innovative methodologies in dendrochronology, case studies on the impact of climate change on tree growth, and reviews of the resilience and adaptation of different tree species. Research on the role of forests in the carbon cycle and tree phenology will also be considered. Additionally, this issue seeks to include interdisciplinary studies that integrate ecology, climatology, and forest management, as well as a focus on conservation policies and recommendations for habitat restoration.

Potential topics include, but are not limited to:

  • Stable isotope analysis;
  • Reconstructions of past climates;
  • Responses of specific species to temperature variations;
  • Effects of drought and water availability;
  • Studies of genetic diversity in relation to climate;
  • Adaptation strategies for changing conditions;
  • Carbon storage in tree rings;
  • The impact of deforestation on the carbon cycle;
  • Effects of storms, wildfires, and frosts on growth.

Prof. Dr. Aldo Rafael Martínez-Sifuentes
Dr. José Villanueva Díaz
Guest Editors

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Keywords

  • tree-ring
  • climate change
  • climatic response
  • adaptation
  • dendrochronology

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Published Papers (2 papers)

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Research

17 pages, 4189 KB  
Article
Tree-Ring Reconstruction of Minimum Temperature Changes in the Northern Greater Khingan Mountains
by Jiabao Xu, Zhaopeng Wang, Dongyou Zhang, Xiangyou Li, Bingyun Du, Xinrui Wang, Kexin Song, Yuanhuan Xie and Zhikuan Liu
Forests 2025, 16(11), 1753; https://doi.org/10.3390/f16111753 - 20 Nov 2025
Cited by 1 | Viewed by 640
Abstract
We established a standardized tree-ring width chronology using 46 Mongolian pine (Pinus sylvestris var. mongolica) tree-ring cores from the Tuqiang Forestry Bureau in the northern Greater Khingan Mountains (GKM). The average minimum temperature from May to July was significantly positively correlated [...] Read more.
We established a standardized tree-ring width chronology using 46 Mongolian pine (Pinus sylvestris var. mongolica) tree-ring cores from the Tuqiang Forestry Bureau in the northern Greater Khingan Mountains (GKM). The average minimum temperature from May to July was significantly positively correlated with tree-ring width, indicating that it is the main climatic factor affecting tree growth in the study area. Based on this, the average minimum temperature sequence from May to July for the past 164 years in this region was reconstructed, and its reliability and stability were verified using the leave-one-out method. The reconstruction results revealed four warm periods and two cold periods in the northern GKM over the past 164 years. The four warm periods were from 1891 to 1897, 1902 to 1909, 1923 to 1931, and 2003 to 2023, and the two cold periods were from 1864 to 1880 and 1953 to 1992. The results of multi-window spectrum analysis and wavelet analysis showed that the reconstructed sequence had periodicities of 2.2–5.3 years, 11 years, 39 years, and 52 years, suggesting that the minimum temperature changes may be influenced by El Niño-Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), and solar sunspot activities. Full article
(This article belongs to the Special Issue Tree-Ring Analysis: Response and Adaptation to Climate Change)
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22 pages, 5340 KB  
Article
Vegetation Growth Carryover and Lagged Climatic Effect at Different Scales: From Tree Rings to the Early Xylem Growth Season
by Jiuqi Chen, Yonghui Wang, Tongwen Zhang, Kexiang Liu, Kailong Guo, Tianhao Hou, Jinghui Song, Zhihao He and Beihua Liang
Forests 2025, 16(7), 1107; https://doi.org/10.3390/f16071107 - 4 Jul 2025
Cited by 1 | Viewed by 912
Abstract
Vegetation growth is influenced not only by current climatic conditions but also by growth-enhancing signals and preceding climate factors. Taking the dominant species, Juniperus seravschanica Kom, in Tajikistan as the research subject, this study combines tree-ring width data with early xylem growth season [...] Read more.
Vegetation growth is influenced not only by current climatic conditions but also by growth-enhancing signals and preceding climate factors. Taking the dominant species, Juniperus seravschanica Kom, in Tajikistan as the research subject, this study combines tree-ring width data with early xylem growth season data (from the start of xylem growth to the first day of the NDVI peak month), simulated using the Vaganov–Shashkin (V-S) model, a process-based tree-ring growth model. This study aims to explore the effects of vegetation growth carryover (VGC) and lagged climatic effects (LCE) on tree rings and the early xylem growth season at two different scales by integrating tree-ring width data and xylem phenology simulations. A vector autoregression (VAR) model was employed to analyze the response intensity and duration of VGC and LCE. The results show that the VGC response intensity in the early xylem growth season is higher than that of tree-ring width. The LCE duration for both the early xylem growth season and tree-ring width ranges from 0 to 11 (years or seasons), with peak LCE response intensity observed at a lag of 2–3 (years or seasons). The persistence of the climate lag effect on vegetation growth has been underestimated, supporting the use of a lag of 0–3 (years or seasons) to study the long-term impacts of climate. The influence of VGC on vegetation growth is significantly stronger than that of LCEs; ultimately indicating that J. seravschanica adapts to harsh environments by modulating its growth strategy through VGC and LCE. Investigating the VGC and LCE of multi-scale xylem growth indicators enhances our understanding of forest ecosystem dynamics. Full article
(This article belongs to the Special Issue Tree-Ring Analysis: Response and Adaptation to Climate Change)
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