Liang et al. (2025) May Relative Humidity Reconstruction Based on Populus cathayana Ring-Width Chronology on the Eastern Tibetan Plateau, China
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Identification
- Journal: Forests
- Year: 2025
- Date: 2025-10-30
- Authors: Zhongwei Liang, Jinbao Li, Tsun Fung Au, Teng Li
- DOI: 10.3390/f16111659
Research Groups
Not specified in the provided text.
Short Summary
This study reconstructed May relative humidity for the eastern Tibetan Plateau over the past 146 years using tree-ring width, revealing multi-decadal variability and its links to ENSO and the East Asian Summer Monsoon.
Objective
- To reconstruct long-term May relative humidity variations on the eastern Tibetan Plateau using tree-ring chronologies to better understand regional climate dynamics and provide a valuable proxy record.
Study Configuration
- Spatial Scale: Eastern Tibetan Plateau.
- Temporal Scale: 160-year tree-ring chronology developed; 146-year reconstruction of May relative humidity (1874–2011).
Methodology and Data
- Models used: Climate-tree growth relationship (statistical model for reconstruction), Spectral analysis.
- Data sources: Tree-ring width chronology from Populus cathayana (proxy data), instrumental May relative humidity (for calibration), other nearby tree-ring records (for validation), EI Nino–Southern Oscillation (ENSO) index, East Asian Summer Monsoon (EASM) index.
Main Results
- A 160-year tree-ring width chronology from Populus cathayana was developed.
- May relative humidity for the eastern Tibetan Plateau was reconstructed for the past 146 years.
- The reconstruction identified three drought periods (1874–1901, 1921–1932, and 2001–2011) and two wet periods (1902–1920 and 1955–2000).
- The reconstructed relative humidity shows high consistency with other regional tree-ring-based temperature and moisture records.
- Spectral analysis detected 2–5 year cycles in relative humidity variability, likely related to ENSO.
- The reconstruction correlates significantly with the East Asian Summer Monsoon (EASM) index, indicating EASM's influence on regional moisture transport.
- The findings highlight the role of ocean–atmosphere coupling in driving humidity variability on the eastern Tibetan Plateau.
Contributions
- Provides the first 146-year May relative humidity reconstruction for the eastern Tibetan Plateau, extending the limited instrumental records.
- Advances understanding of long-term regional climate dynamics and moisture variability.
- Offers a valuable proxy record for future climate change assessments and paleoclimate studies.
- Identifies teleconnections between regional humidity and large-scale climate phenomena (ENSO, EASM).
Funding
Not specified in the provided text.
Citation
@article{Liang2025May,
author = {Liang, Zhongwei and Li, Jinbao and Au, Tsun Fung and Li, Teng},
title = {May Relative Humidity Reconstruction Based on Populus cathayana Ring-Width Chronology on the Eastern Tibetan Plateau, China},
journal = {Forests},
year = {2025},
doi = {10.3390/f16111659},
url = {https://doi.org/10.3390/f16111659}
}
Original Source: https://doi.org/10.3390/f16111659