Articles | Volume 17, issue 13
Atmos. Chem. Phys., 17, 8177–8187, 2017
https://doi.org/10.5194/acp-17-8177-2017
Atmos. Chem. Phys., 17, 8177–8187, 2017
https://doi.org/10.5194/acp-17-8177-2017

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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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Svenja Lange on behalf of the Authors (29 May 2017)  Author's response    Manuscript
ED: Publish as is (29 May 2017) by Armin Sorooshian
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Short summary
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.
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