Deconvolution of boundary layer depth and aerosol constraints on cloud water path in subtropical stratocumulus decks

Possner, Anna; Eastman, Ryan; Bender, Frida; Glassmeier, Franziska

doi:https://doi.org/10.5194/acp-20-3609-2020

Articles | Volume 20, issue 6

https://doi.org/10.5194/acp-20-3609-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/acp-20-3609-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 20, issue 6

Research article

| Highlight paper

|

26 Mar 2020

Research article | Highlight paper |

| 26 Mar 2020

Deconvolution of boundary layer depth and aerosol constraints on cloud water path in subtropical stratocumulus decks

Anna Possner, Ryan Eastman, Frida Bender, and Franziska Glassmeier

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Final revised paper (published on 26 Mar 2020)
Supplement to the final revised paper
Preprint (discussion started on 17 Oct 2019)
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Interactive discussion

Status: closed

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

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RC1: 'Comments on: Deconvolution of Boundary Layer Depth and Aerosol Constraints on Cloud Water Path in Subtropical Stratocumuli', Anonymous Referee #1, 21 Oct 2019
RC2: 'Review of ACP-2019-833', Anonymous Referee #2, 05 Nov 2019
AC1: 'Authur Response for Reviews on "Deconvolution of Boundary Layer Depth and Aerosol Constraints on Cloud Water Path in Subtropical Stratocumulus decks"', Anna Possner, 07 Feb 2020

Peer-review completion

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

AR by Anna Possner on behalf of the Authors (10 Feb 2020) Manuscript

ED: Referee Nomination & Report Request started (14 Feb 2020) by Johannes Quaas

RR by Anonymous Referee #2 (25 Feb 2020)

ED: Publish subject to technical corrections (25 Feb 2020) by Johannes Quaas

AR by Anna Possner on behalf of the Authors (26 Feb 2020) Author's response Manuscript

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Short summary

Cloud water content and the number of droplets inside clouds covary with boundary layer depth. This covariation may amplify the change in water content due to a change in droplet number inferred from long-term observations. Taking this into account shows that the change in water content for increased droplet number in observations and high-resolution simulations agrees in shallow boundary layers. Meanwhile, deep boundary layers are under-sampled in process-scale simulations and observations.