Forest canopy interactions with nucleation mode particles

Pryor, S. C.; Hornsby, K. E.; Novick, K. A.

doi:https://doi.org/10.5194/acp-14-11985-2014

Articles | Volume 14, issue 21

https://doi.org/10.5194/acp-14-11985-2014

© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

https://doi.org/10.5194/acp-14-11985-2014

© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 14, issue 21

Research article

|

14 Nov 2014

Research article |

| 14 Nov 2014

Forest canopy interactions with nucleation mode particles

S. C. Pryor, K. E. Hornsby, and K. A. Novick

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Final revised paper (published on 14 Nov 2014)
Preprint (discussion started on 04 Jul 2014)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC C6167: 'reivew', Anonymous Referee #1, 25 Aug 2014
- AC C7072: 'Detailed response to reviewers comments', Sara C. Pryor, 15 Sep 2014
RC C6170: 'referee comments', Anonymous Referee #2, 25 Aug 2014
- AC C7080: 'Detailed response to reviewers comments', Sara C. Pryor, 15 Sep 2014

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

AR by Sara C. Pryor on behalf of the Authors (29 Sep 2014) Author's response

ED: Publish as is (06 Oct 2014) by Fangqun Yu

Short summary

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.