Observational Constraints and Attribution of Global Plant Transpiration Changes Over the Past Four Decades

Author:

Cui Jiangpeng1ORCID,Ding Jinzhi1,Lian Xu2ORCID,Wei Zhongwang34ORCID,Li Shijie5,Peng Jian67,Poyatos Rafael89ORCID,Wang Tao1ORCID,Piao Shilong110ORCID

Affiliation:

1. State Key Laboratory of Tibetan Plateau Earth System and Resources Environment (TPESRE) Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing China

2. Department of Earth and Environmental Engineering Columbia University New York NY USA

3. Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies School of Atmospheric Sciences Sun Yat‐Sen University Guangzhou China

4. Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai) Zhuhai China

5. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters Nanjing University of Information Science and Technology Nanjing China

6. Department of Remote Sensing Helmholtz Centre for Environmental Research—UFZ Leipzig Germany

7. Remote Sensing Centre for Earth System Research Leipzig University Leipzig Germany

8. CREAF Barcelona Spain

9. Universitat Autònoma de Barcelona Barcelona Spain

10. Institute of Carbon Neutrality Sino‐French Institute for Earth System Science College of Urban and Environmental Sciences Peking University Beijing China

Abstract

AbstractAccurate estimation and attribution of large‐scale changes in plant transpiration are critical to understand the impacts of vegetation dynamics on the terrestrial hydrological cycle. However, these aspects remain poorly understood due to the limited reliability of global transpiration products. Here we compile data from 101 site‐based transpiration measurements across the globe and use them to constrain three biophysically based data‐driven transpiration products. The constrained transpiration reveals a prominent increasing trend of 0.61–0.79 mm yr−2 during 1980–2021, which is overestimated by 8%–32% in unconstrained transpiration. We further find that the global transpiration increase is mainly driven by leaf area index increase (40%), followed by climate change (19%), though offset partly by CO2‐induced stomatal closure (−38%) and land use and cover change (−3%). Our refined estimates indicate a less substantial increase of global transpiration than previously thought, improving the understanding of transpiration change impact on global hydrological cycle.

Publisher

American Geophysical Union (AGU)

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