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Enhanced global primary production by biogenic aerosol via diffuse radiation fertilization

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posted on 2025-07-31, 22:43 authored by A Rap, CE Scott, CL Reddington, L Mercado, RJ Ellis, S Garraway, MJ Evans, DJ Beerling, AR MacKenzie, CN Hewitt, DV Spracklen
Terrestrial vegetation releases large quantities of plant volatiles into the atmosphere that can then oxidize to form secondary organic aerosol. These particles affect plant productivity through the diffuse radiation fertilization effect by altering the balance between direct and diffuse radiation reaching the Earth’s surface. Here, using a suite of models describing relevant coupled components of the Earth system, we quantify the impacts of biogenic secondary organic aerosol on plant photosynthesis through this fertilization effect. We show that this leads to a net primary productivity enhancement of 1.23 Pg C yr−1(range 0.76–1.61 Pg C yr−1due to uncertainty in biogenic secondary organic aerosol formation). Notably, this productivity enhancement is twice the mass of biogenic volatile organic compound emissions (and ~30 times larger than the mass of carbon in biogenic secondary organic aerosol) causing it. Hence, our simulations indicate that there is a strong positive ecosystem feedback between biogenic volatile organic compound emissions and plant productivity through plant-canopy light-use efficiency. We estimate a gain of 1.07 in global biogenic volatile organic compound emissions resulting from this feedback.

Funding

We acknowledge funding from the Natural Environment Research Council (NE/J004723/1, NE/J009822/1 and NE/K015966/1) and EU Horizon 2020 (SC5-01-2014; grant agreement 641816). D.V.S. acknowledges support from a Philip Leverhulme Prize and C.N.H. thanks Lancaster University for funding.

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© 2018 The Author(s)

Notes

This is the author accepted manuscript. The final version is available from Springer Nature via the DOI in this record Data availability: The AERONET remote-sensed data are publicly available from https://aeronet.gsfc.nasa.gov/. Data from our model simulations are available from the corresponding author upon request. Code availability: Requests for the radiative transfer and land-surface models used to generate these results can be made via https://code.metoffice.gov.uk/trac/home and http://jules.jchmr.org/, respectively.

Journal

Nature Geoscience

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Springer Nature

Language

en

Citation

Vol. 11, pp. 640 - 644

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