J Plant Ecol ›› 2026, Vol. 19 ›› Issue (3): rtaf195.DOI: 10.1093/jpe/rtaf195

• Research Article •    

Nitrogen deposition altered the climatic sensitivity of vegetation phenology

Yuzhu Chen1, Peng Li1,*, Yunpeng Luo2, Longjun Wang1, Ying Peng1, Tong Li1, Xiaolu Zhou1,*, Changhui Peng1,3   

  1. 1College of Geographic Science, Hunan Normal University, Changsha 410081, China, 2Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Birmensdorf 8903, Switzerland, 3Department of Biological Sciences, University of Québec at Montreal, Montreal, Canada

    *Corresponding authors. E-mails: lipeng2019@hunnu.edu.cn(P.L.); zhoux1977@163.com(X.Z.)

  • Received:2025-09-03 Accepted:2025-11-06 Online:2025-11-18 Published:2026-06-01
  • Supported by:
    This study was financially supported by the National Natural Science Foundation of China (Grants 42371121, U22A20570); Natural Science Foundation of Hunan Province, China (Grant 2024JJ5262).

氮沉降改变植被物候气候敏感性

Abstract: Nitrogen deposition substantially alters nutrient absorption by plant root systems, which has far-reaching consequences for leaf growth and development. However, its effects on plant phenology and climatic sensitivity remain unclear. This study investigated the effects of nitrogen deposition on vegetation phenology and its sensitivity to moisture and temperature from 1982 to 2022 by combining data from field experiments, remote-sensing observations, and land surface models. The results revealed that the start of the growing season (SOS) has become more sensitive to vapor pressure deficit (VPD), whereas its sensitivity to temperature and soil moisture (SM) has decreased in recent decades. Conversely, there was no notable trend in climatic sensitivity at the end of the growing season (EOS). The model results show that SOS’s sensitivity to VPD (SVPD) and temperature (STem) increased with higher nitrogen deposition levels (SVPD, a = 1.07 d unit−1, P < 0.01; STem, a = 0.10 d unit−1, P < 0.01). The sensitivity of EOS to soil moisture (SSM) decreased significantly with increasing nitrogen deposition (a = −1.82 d unit−1, P < 0.05), whereas SVPD decreased (a = −0.38 d unit−1, P < 0.01). Attribution analysis indicated that nitrogen deposition was the primary driver of changes in the climatic sensitivity of SOS, whereas atmospheric CO2 predominantly influenced changes in the SSM of EOS. These results emphasize the critical role of nitrogen deposition in determining the climatic sensitivity of vegetation phenology and provide a novel perspective for understanding and predicting vegetation phenology dynamics under ongoing global change.

The study reveals that nitrogen deposition amplifies spring phenology sensitivity to VPD and reducing its sensitivity to temperature and soil moisture, whereas no marked effect was observed on autumn phenology. This finding highlights the critical regulatory role of nitrogen deposition in phenological climate responses, holding important implications for predicting phenological dynamics under global change.

Key words: carbon cycle, climatic sensitivity, global change, nitrogen deposition, vegetation phenology

摘要:
氮沉降显著改变了植物养分吸收,从而影响叶片生长与发育过程。然而,氮沉降如何影响植被物候及其气候敏感性,目前尚缺乏系统认识。本研究结合野外实验、遥感观测和陆面模型,解析了1982–2022年间北半球中高纬度地区氮沉降对植被物候及其水分和温度敏感性的影响。结果表明,近40年来,生长季开始期(SOS)对饱和水汽压差(VPD)的敏感性增强,而对温度和土壤湿度(SM)的敏感性则有所减弱;相比之下,生长季结束期(EOS)的气候敏感性并未表现出显著变化趋势。模型模拟显示,随着氮沉降速率的升高,SOS对VPD (SVPD)和温度(STem)的敏感性均显著增强(SVPD, a =1.07 d unit−1P < 0.01; STem, a = 0.10 d unit−1, P < 0.01);而EOS对SM的敏感性(SSM)随氮沉降增加则显著减弱(a = −1.82 d unit−1, P < 0.05),SVPD呈下降趋势(a = −0.38 d unit−1, P < 0.01)。归因分析表明,氮沉降是导致SOS气候敏感性变化的主要驱动因子,而大气CO2浓度上升主要影响了EOS对SSM的敏感性。本研究强调了氮沉降在调控植被物候气候敏感性中的关键作用,为深入理解和预测全球变化背景下植被物候动态提供了新视角。

关键词: 碳循环, 气候敏感性, 全球变化, 氮沉降, 植被物候