Abstract
UNDERSTANDING mass and energy exchange between vegetation and the atmosphere is essential for determining the future state of the climate system1,2 and responses of plant communities. Plant water use is at present described by steady-state transport models3,4, even though transport in the boundary layer is turbulent5,6. This is especially true for forests, where the canopy air space is a chaotic environment where large turbulent events alternate with smaller-scale mixing3,4,7. Here we demonstrate that the turbulent nature of the atmosphere affects plant processes. We propose that the dynamic nature of plant-atmosphere coupling represents a previously unrecognized feedback that influences plant water use and transport.
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Hollinger, D., Kelliher, F., Schulze, ED. et al. Coupling of tree transpiration to atmospheric turbulence. Nature 371, 60–62 (1994). https://doi.org/10.1038/371060a0
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DOI: https://doi.org/10.1038/371060a0
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