Trends and Climate‐Sensitivity of Phenology in China's Natural and Planted Forests

Author:

Xian Ziyi123ORCID,Yu Zhen123ORCID,Agathokleous Evgenios123,Han Wangya23ORCID,You Weibin4,Zhou Guoyi23ORCID

Affiliation:

1. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC‐FEMD) Nanjing University of Information Science & Technology Nanjing China

2. Key Laboratory of Ecosystem Carbon Source and Sink China Meteorological Administration (ECSS‐CMA) School of Ecology and Applied Meteorology Nanjing University of Information Science and Technology Nanjing China

3. Institute of Ecology School of Ecology and Applied Meteorology Nanjing University of Information Science & Technology Nanjing China

4. College of Forestry Fujian Agriculture and Forestry University Fuzhou China

Abstract

AbstractForest is the largest carbon sink on land, and the timing of forest phenology profoundly influences carbon uptake. However, disparities in the timing and sensitivity of forest phenology, particularly between planted forests (PF) and natural forests (NF), have yet to be determined. In this study, we analyzed the phenological trends and the climate‐sensitivities of China's NF and PF from 2000 to 2022 using field survey data and satellite data. We found that the start of the growing season (start of the season (SOS)) in NF and PF advanced significantly by 0.07 and 0.08 days yr−1, while the end of the growing season (end of the season (EOS)) in both NF and PF delayed by 0.06 days yr−1. Moreover, precipitation and air temperature jointly influenced the timing of phenological events. The pre‐season precipitation delayed the EOS by 0.009 days mm−1 and 0.006 days mm−1 in NF and PF. Moreover, the SOS was more sensitive to precipitation in PF than in NF in arid areas (i.e., pre‐season precipitation <100 mm). Air temperature significantly advanced the SOS by 0.74 and 0.95 days °C−1 in NF and PF and delayed the EOS by 0.89 and 0.71 days °C−1 in NF and PF. Additionally, the sensitivities of SOS and EOS to air temperature significantly differed between NF and PF. Our findings demonstrate a significant phenological discrepancy between PF and NF. The results suggest that NF and PF responded differently to climate variability, implying forest origin should be considered in the projection of carbon sequestration capability under changing climate.

Funder

National Natural Science Foundation of China

National Key Research and Development Program of China

Publisher

American Geophysical Union (AGU)

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