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Volume 17, issue 13
Atmos. Chem. Phys., 17, 8177–8187, 2017
https://doi.org/10.5194/acp-17-8177-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 17, 8177–8187, 2017
https://doi.org/10.5194/acp-17-8177-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 05 Jul 2017

Research article | 05 Jul 2017

The boundary condition for vertical velocity and its interdependence with surface gas exchange

Andrew S. Kowalski

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Cited articles

Aaltonen, H., Pumpanen, J., Pihlatie, M., Hakola, H., Hellén, H., Kulmala, L., Vesala, T., and Bäck, J.: Boreal pine forest floor biogenic volatile organic compound emissions peak in early summer and autumn, Agr. Forest Meteorol., 151, 682–691, https://doi.org/10.1016/j.agrformet.2010.12.010, 2011.
Abramzon, B. and Sirignano, W. A.: Droplet vaporization model for spray compustion calculations, Int. J. Heat Mass Tran., 32, 1605–1618, 1989.
Arya, S. P.: Introduction to Micrometeorology, Academic Press, San Diego, 307 pp., 1988.
Bird, R. B., Stewart, W. E., and Lightfoot, E. N.: Transport Phenomena, John Wiley & Sons, Cambridge, 2002.
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An analysis based on physical conservation law demonstrates that surface–atmosphere exchanges include a non-diffusive component. This implies the need to revise flux gradient relationships including eddy diffusivities in micrometeorology and stomatal conductances in plant physiology.
An analysis based on physical conservation law demonstrates that surface–atmosphere exchanges...
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