Dominant role of the non‐forest woody vegetation in the post 2015/16 El Niño tropical carbon recovery

Author:

Fan Lei1,Cui Tianxiang2ORCID,Wigneron Jean‐Pierre3ORCID,Ciais Philippe4,Sitch Stephen5,Brandt Martin6,Li Xin7,Niu Shuli89ORCID,Xiao Xiangming10ORCID,Chave Jérome11ORCID,Wu Chaoyang12,Li Wei13ORCID,Yuan Wenping14,Xing Zanpin315,Li Xiaojun3,Wang Mengjia16,Liu Xiangzhuo3,Chen Xiuzhi17ORCID,Qin Yuanwei10,Yang Hui18ORCID,Tang Qiang1,Li Yuechen1,Ma Mingguo1,Fensholt Rasmus6

Affiliation:

1. Chongqing Jinfo Mountain Karst Ecosystem National Observation and Research Station, School of Geographical Sciences Southwest University Chongqing China

2. Co‐Innovation Center for Sustainable Forestry in Southern China Nanjing Forestry University Nanjing China

3. INRAE, Bordeaux Sciences Agro, UMR 1391 ISPA Villenave‐d'Ornon France

4. Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA‐CNRS‐UVSQ Université Paris‐Saclay Gif‐sur‐Yvette France

5. College of Life and Environmental Sciences University of Exeter Exeter UK

6. Department of Geosciences and Natural Resource Management University of Copenhagen Copenhagen Denmark

7. Environment and Resources (TPESER), Institute of Tibetan Plateau Research Chinese Academy of Sciences Beijing China

8. Key Laboratory of Ecosystem Network Observation and Simulation, Institute of Geographical Sciences and Natural Resources Research Chinese Academy of Sciences Beijing China

9. College of Resources and Environment University of Chinese Academy of Sciences Beijing China

10. Plant Biology, Center for Earth Observation and Modeling University of Oklahoma Norman Oklahoma USA

11. Diversité Biologique, CNRS, IRD, UT3 Université Paul Sabatier Toulouse France

12. Institute of Geographical Sciences and Natural Resources Research Chinese Academy of Sciences Beijing China

13. Ministry of Education Key Laboratory for Earth System Modeling, Department of Earth System Science Tsinghua University Beijing China

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

15. Cryosphere Research Station on the Qinghai‐Tibet Plateau, State Key Laboratory of Cryospheric Science, Northwest Institute of Eco‐Environment and Resource Chinese Academy of Sciences Lanzhou China

16. School of Geoscience and Technology Zhengzhou University Zhengzhou China

17. Climate Change and Natural Disaster Studies, School of Atmospheric Sciences Sun Yat‐sen University Guangzhou China

18. Department of Biogeochemical Integration Max Planck Institute for Biogeochemistry Jena Germany

Abstract

AbstractThe extreme dry and hot 2015/16 El Niño episode caused large losses in tropical live aboveground carbon (AGC) stocks. Followed by climatic conditions conducive to high vegetation productivity since 2016, tropical AGC are expected to recover from large losses during the El Niño episode; however, the recovery rate and its spatial distribution remain unknown. Here, we used low‐frequency microwave satellite data to track AGC changes, and showed that tropical AGC stocks returned to pre‐El Niño levels by the end of 2020, resulting in an AGC sink of Pg C year−1 during 2014–2020. This sink was dominated by strong AGC increases ( Pg C year−1) in non‐forest woody vegetation during 2016–2020, compensating the forest AGC losses attributed to the El Niño event, forest loss, and degradation. Our findings highlight that non‐forest woody vegetation is an increasingly important contributor to interannual to decadal variability in the global carbon cycle.

Funder

National Science Foundation

National Natural Science Foundation of China

Publisher

Wiley

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