- Research Article
- 10.1038/s41477-026-02304-w
Leaf temperature and its departure from ambient air temperature.
- May 08, 2026
- Nature plants
- Xu Lian + 15 more +15
Leaf temperature (Tl), the temperature at which leaf-air exchanges of carbon and water occur, varies with ambient air temperature (Ta), regulated by microclimate and species' energy balance traits. Ground and satellite thermal measurements of the Tl-Ta relationship are widely used to infer plants' thermoregulation capacity. On the basis of a global synthesis of observations across diverse climates and biomes, we show that reported thermoregulation patterns vary primarily along temperature gradients. Megathermy (dTl/dTa > 1) is particularly prevalent in warm tropical regions and in sun-exposed canopy-top leaves owing to ineffective dissipation of the often excessively accumulated solar radiation, while limited homeothermy (dTl/dTa < 1) and poikilothermy (dTl/dTa = 1) are reported mostly for cold ecosystems or sub-canopy leaves. Under heat-stressed conditions, some warm-adapted species can abate rapid Tl surge through active stomatal control, unless critical temperature thresholds are exceeded, above which Tl might increase non-linearly as a warning sign of damaging stress. This thermal consideration of stomatal regulation is currently missing in mechanistic models as a source of bias in estimated photosynthetic rates. We highlight the pressing need to develop new stomatal theories that tackle a triple-target optimization between carbon gain, water loss and thermal regulation.
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