The browser you are using is not supported by this website. All versions of Internet Explorer are no longer supported, either by us or Microsoft (read more here: https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Please use a modern browser to fully experience our website, such as the newest versions of Edge, Chrome, Firefox or Safari etc.

jing tang profile picture

Jing Tang

Researcher

jing tang profile picture

Global warming is increasing the discrepancy between green (actual) and thermal (potential) seasons of temperate trees

Author

  • Yongshuo H. Fu
  • Xiaojun Geng
  • Shouzhi Chen
  • Hao Wu
  • Fanghua Hao
  • Xuan Zhang
  • Zhaofei Wu
  • Jing Zhang
  • Jing Tang
  • Yann Vitasse
  • Constantin M. Zohner
  • Ivan Janssens
  • Nils Chr Stenseth
  • Josep Peñuelas

Summary, in English

Over the past decades, global warming has led to a lengthening of the time window during which temperatures remain favorable for carbon assimilation and tree growth, resulting in a lengthening of the green season. The extent to which forest green seasons have tracked the lengthening of this favorable period under climate warming, however, has not been quantified to date. Here, we used remote sensing data and long-term ground observations of leaf-out and coloration for six dominant species of European trees at 1773 sites, for a total of 6060 species–site combinations, during 1980–2016 and found that actual green season extensions (GS: 3.1 ± 0.1 day decade−1) lag four times behind extensions of the potential thermal season (TS: 12.6 ± 0.1 day decade−1). Similar but less pronounced differences were obtained using satellite-derived vegetation phenology observations, that is, a lengthening of 4.4 ± 0.13 and 7.5 ± 0.13 day decade−1 for GS and TS, respectively. This difference was mainly driven by the larger advance in the onset of the thermal season compared to the actual advance of leaf-out dates (spring mismatch: 7.2 ± 0.1 day decade−1), but to a less extent caused by a phenological mismatch between GS and TS in autumn (2.4 ± 0.1 day decade−1). Our results showed that forest trees do not linearly track the new thermal window extension, indicating more complex interactions between winter and spring temperatures and photoperiod and a justification of demonstrating that using more sophisticated models that include the influence of chilling and photoperiod is needed to accurately predict spring phenological changes under warmer climate. They urge caution if such mechanisms are omitted to predict, for example, how vegetative health and growth, species distribution and crop yields will change in the future.

Department/s

  • Dept of Physical Geography and Ecosystem Science
  • MERGE: ModElling the Regional and Global Earth system

Publishing year

2023

Language

English

Pages

1377-1389

Publication/Series

Global Change Biology

Volume

29

Issue

5

Document type

Journal article

Publisher

Wiley-Blackwell

Topic

  • Ecology
  • Climate Research

Keywords

  • autumnal foliar senescence
  • climatic warming
  • green season
  • spring leaf-out
  • thermal season

Status

Published

ISBN/ISSN/Other

  • ISSN: 1354-1013