Aerosol characteristics in the entrainment interface layer in relation to the marine boundary layer and free troposphere

Dadashazar, Hossein; Braun, Rachel A.; Crosbie, Ewan; Chuang, Patrick Y.; Woods, Roy K.; Jonsson, Haflidi H.; Sorooshian, Armin

doi:https://doi.org/10.5194/acp-18-1495-2018

Articles | Volume 18, issue 3

https://doi.org/10.5194/acp-18-1495-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-18-1495-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 18, issue 3

Research article

|

02 Feb 2018

Research article |

| 02 Feb 2018

Aerosol characteristics in the entrainment interface layer in relation to the marine boundary layer and free troposphere

Hossein Dadashazar, Rachel A. Braun, Ewan Crosbie, Patrick Y. Chuang, Roy K. Woods, Haflidi H. Jonsson, and Armin Sorooshian

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Final revised paper (published on 02 Feb 2018)
Preprint (discussion started on 06 Oct 2017)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Reviewer Comments', Anonymous Referee #1, 06 Nov 2017
RC2: 'Review', Anonymous Referee #2, 10 Dec 2017
AC1: 'Response to referee 1', Hossein Dadashazar, 26 Dec 2017
AC2: 'Response to referee 2', Hossein Dadashazar, 26 Dec 2017

Peer-review completion

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

AR by Hossein Dadashazar on behalf of the Authors (26 Dec 2017) Author's response Manuscript

ED: Publish as is (03 Jan 2018) by Manabu Shiraiwa

AR by Hossein Dadashazar on behalf of the Authors (03 Jan 2018)

Short summary

This study shows with airborne data that in the thin layer above stratocumulus clouds, the entrainment interface layer (EIL), aerosol size distributions are influenced both by new particle formation and by pollutants above and below the EIL. These results are important with regard to understanding aerosol–cloud–climate interactions as the aerosol in this layer can influence the characteristics of stratocumulus clouds, which are the dominant cloud type by global area.