Impact of the 2015/2016 El Niño on the terrestrial carbon cycle constrained by bottom-up and top-down approaches
- Ludwig Maximilians Univ. Munich, Munich (Germany); Lab. des Sciences du Climat et de l'Environnement (LSCE), Gif-sur-Yvette (France)
- Univ. of Exeter, Exeter (United Kingdom)
- Boston Univ., Boston, MA (United States)
- Univ. de Toulouse, Toulouse (France)
- Centre Bordeaux Aquitaine, Villenave d'Ornon (France)
- Univ. of Victoria, Victoria, BC (Canada)
- CSIRO Oceans and Atmosphere, Canberra, ACT (Australia)
- Lab. des Sciences du Climat et de l'Environnement (LSCE), Gif-sur-Yvette (France)
- Wuhan Univ., Wuhan (People's Republic of China)
- CNRS/Meteo-France/Univ. Federale de Toulouse, Toulouse (France)
- Univ. of Illinois, Urbana, IL (United States)
- Univ. of Bern, Bern (Switzerland)
- Institute of Applied Energy (IAE), Tokyo (Japan)
- National Center for Atmospheric Research, Boulder, CO (United States)
- Environment and Climate Change Canada, Downsview, ON (Canada)
- Max Planck Institute for Meteorology, Hamburg (Germany)
- Ludwig Maximilians Univ. Munich, Munich (Germany); Max Planck Institute for Meteorology, Hamburg (Germany)
- NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
- Max Planck Institute for Biogeochemistry, Jena (Germany)
- Auburn Univ., Auburn, AL (United States)
- Univ. Libre de Bruxelles, Brussels (Belgium)
- Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
- Met Office Hadley Centre, Exeter (United Kingdom)
- Univ. of Maryland, College Park, MD (United States); Institute of Atmospheric Physics, Beijing (People's Republic of China)
Evaluating the response of the land carbon sink to the anomalies in temperature and drought imposed by El Niño events provides insights into the present-day carbon cycle and its climate-driven variability. It is also a necessary step to build confidence in terrestrial ecosystems models' response to the warming and drying stresses expected in the future over many continents, and particularly in the tropics. Here we present an in-depth analysis of the response of the terrestrial carbon cycle to the 2015/2016 El Niño that imposed extreme warming and dry conditions in the tropics and other sensitive regions. First, we provide a synthesis of the spatio-temporal evolution of anomalies in net land–atmosphere CO2 fluxes estimated by two in situ measurements based on atmospheric inversions and 16 land-surface models (LSMs) from TRENDYv6. Simulated changes in ecosystem productivity, decomposition rates and fire emissions are also investigated. Inversions and LSMs generally agree on the decrease and subsequent recovery of the land sink in response to the onset, peak and demise of El Niño conditions and point to the decreased strength of the land carbon sink: by 0.4–0.7 PgC yr–1 (inversions) and by 1.0 PgC yr–1 (LSMs) during 2015/2016. As a result, LSM simulations indicate that a decrease in productivity, rather than increase in respiration, dominated the net biome productivity anomalies in response to ENSO throughout the tropics, mainly associated with prolonged drought conditions.
- Research Organization:
- Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
- Sponsoring Organization:
- USDOE Office of Science (SC), Biological and Environmental Research (BER)
- Grant/Contract Number:
- AC05-00OR22725
- OSTI ID:
- 1484986
- Journal Information:
- Philosophical Transactions of the Royal Society of London, Series B: Biological Sciences, Vol. 373, Issue 1760; ISSN 0962-8436
- Publisher:
- The Royal Society PublishingCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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