On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface

Freda, Włodzimierz; Haule, Kamila; Sagan, Sławomir

doi:https://doi.org/10.5194/os-15-745-2019

Articles | Volume 15, issue 3

https://doi.org/10.5194/os-15-745-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/os-15-745-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 15, issue 3

Research article

|

17 Jun 2019

Research article |

| 17 Jun 2019

On the role of the seawater absorption-to-attenuation ratio in the radiance polarization above the southern Baltic surface

Włodzimierz Freda, Kamila Haule, and Sławomir Sagan

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Final revised paper (published on 17 Jun 2019)
Preprint (discussion started on 28 Nov 2018)

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of os-2018-127', Anonymous Referee #1, 24 Jan 2019
- AC1: 'Answer to review 1', Włodzimierz Freda, 26 Feb 2019
- AC2: 'Attached file with corrections added', Włodzimierz Freda, 26 Feb 2019
RC2: 'Re-review', Anonymous Referee #2, 08 Mar 2019
- AC3: 'Respond to Reviewer 2', Włodzimierz Freda, 05 Apr 2019

Peer-review completion

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

AR by Włodzimierz Freda on behalf of the Authors (29 Apr 2019) Author's response Manuscript

ED: Referee Nomination & Report Request started (02 May 2019) by Oliver Zielinski

RR by Anonymous Referee #2 (02 May 2019)

ED: Publish as is (02 May 2019) by Oliver Zielinski

Short summary

The paper presents a correlation that can potentially improve the signal obtained from ocean color remote sensing. Results come from a modeling applied to the atmosphere–ocean system in different regions of the southern Baltic, two seasons and two wind speeds, each for nine visible spectral bands. The results show that the variability of the maximum of DoP depends more on seasonal than regional changes and can be explained to a large degree by the seawater absorption-to-attenuation ratio.