Articles | Volume 14, issue 21
Atmos. Chem. Phys., 14, 11985–11996, 2014
https://doi.org/10.5194/acp-14-11985-2014
Atmos. Chem. Phys., 14, 11985–11996, 2014
https://doi.org/10.5194/acp-14-11985-2014
Research article
14 Nov 2014
Research article | 14 Nov 2014

Forest canopy interactions with nucleation mode particles

S. C. Pryor et al.

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Cited articles

Abrams, M. D.: Where Has All the White Oak Gone?, BioScience, 53, 927–939, 2003.
Barthelmie, R. J. and Pryor, S. C.: A model mechanism to describe oxidation of monoterpenes leading to secondary organic aerosol 1. α-pinene and β-pinene, J. Geophys. Res., 104, 23657–23699, 1999.
Boy, M. and Kulmala, M.: Nucleation events in the continental boundary layer: Influence of physical and meteorological parameters, Atmos. Chem. Phys., 2, 1–16, https://doi.org/10.5194/acp-2-1-2002, 2002.
Burkhardt, J., Basi, S., Pariyar, S., and Hunsche, M.: Stomatal penetration by aqueous solutions – an update involving leaf surface particles, New Phytol., 196, 774–787, 2012.
Bzdek, B. R., Zordan, C. A., Pennington, M. R., Luther, G. W., and Johnston, M. V.: Quantitative Assessment of the Sulfuric Acid Contribution to New Particle Growth, Environ. Sci. Technol., 46, 4365–4373, 2012.
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What role do forests play in determining the concentration (and composition) of climate-relevant aerosol particles? This study seeks to address two aspects of this question. Firstly, we document high in-canopy removal of recently formed particles. Then we show evidence that growth rates of particles are a function of soil water availability via a reduction in canopy emissions of gases responsible for particle growth to climate-relevant sizes during drought conditions.
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