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Tropical forests are approaching critical temperature thresholds

Author

Listed:
  • Christopher E. Doughty

    (Northern Arizona University)

  • Jenna M. Keany

    (Northern Arizona University)

  • Benjamin C. Wiebe

    (Northern Arizona University)

  • Camilo Rey-Sanchez

    (North Carolina State University)

  • Kelsey R. Carter

    (Michigan Technological University
    Earth and Environmental Sciences Division, Los Alamos National Laboratory)

  • Kali B. Middleby

    (James Cook University)

  • Alexander W. Cheesman

    (James Cook University)

  • Michael L. Goulden

    (University of California)

  • Humberto R. Rocha

    (Universidade de São Paulo)

  • Scott D. Miller

    (State University of New York at Albany)

  • Yadvinder Malhi

    (University of Oxford)

  • Sophie Fauset

    (University of Plymouth)

  • Emanuel Gloor

    (University of Leeds)

  • Martijn Slot

    (Smithsonian Tropical Research Institute, Balboa)

  • Imma Oliveras Menor

    (University of Oxford
    AMAP (Botanique et Modélisation de l’Architecture des Plantes et des Végétations), CIRAD, CNRS, INRA, IRD, Université de Montpellier)

  • Kristine Y. Crous

    (Western Sydney University, Hawkesbury Institute for the Environment)

  • Gregory R. Goldsmith

    (Chapman University)

  • Joshua B. Fisher

    (Chapman University)

Abstract

The critical temperature beyond which photosynthetic machinery in tropical trees begins to fail averages approximately 46.7 °C (Tcrit)1. However, it remains unclear whether leaf temperatures experienced by tropical vegetation approach this threshold or soon will under climate change. Here we found that pantropical canopy temperatures independently triangulated from individual leaf thermocouples, pyrgeometers and remote sensing (ECOSTRESS) have midday peak temperatures of approximately 34 °C during dry periods, with a long high-temperature tail that can exceed 40 °C. Leaf thermocouple data from multiple sites across the tropics suggest that even within pixels of moderate temperatures, upper canopy leaves exceed Tcrit 0.01% of the time. Furthermore, upper canopy leaf warming experiments (+2, 3 and 4 °C in Brazil, Puerto Rico and Australia, respectively) increased leaf temperatures non-linearly, with peak leaf temperatures exceeding Tcrit 1.3% of the time (11% for more than 43.5 °C, and 0.3% for more than 49.9 °C). Using an empirical model incorporating these dynamics (validated with warming experiment data), we found that tropical forests can withstand up to a 3.9 ± 0.5 °C increase in air temperatures before a potential tipping point in metabolic function, but remaining uncertainty in the plasticity and range of Tcrit in tropical trees and the effect of leaf death on tree death could drastically change this prediction. The 4.0 °C estimate is within the ‘worst-case scenario’ (representative concentration pathway (RCP) 8.5) of climate change predictions2 for tropical forests and therefore it is still within our power to decide (for example, by not taking the RCP 6.0 or 8.5 route) the fate of these critical realms of carbon, water and biodiversity3,4.

Suggested Citation

  • Christopher E. Doughty & Jenna M. Keany & Benjamin C. Wiebe & Camilo Rey-Sanchez & Kelsey R. Carter & Kali B. Middleby & Alexander W. Cheesman & Michael L. Goulden & Humberto R. Rocha & Scott D. Mille, 2023. "Tropical forests are approaching critical temperature thresholds," Nature, Nature, vol. 621(7977), pages 105-111, September.
  • Handle: RePEc:nat:nature:v:621:y:2023:i:7977:d:10.1038_s41586-023-06391-z
    DOI: 10.1038/s41586-023-06391-z
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