Atmospheric water-soluble organic nitrogen (WSON) in the eastern Mediterranean: origin and ramifications regarding marine productivity

Nehir, Münevver; Koçak, Mustafa

doi:https://doi.org/10.5194/acp-18-3603-2018

Articles | Volume 18, issue 5

https://doi.org/10.5194/acp-18-3603-2018

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

Special issue:

CHemistry and AeRosols Mediterranean EXperiments (ChArMEx)...

https://doi.org/10.5194/acp-18-3603-2018

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

Articles | Volume 18, issue 5

Research article

|

13 Mar 2018

Research article |

| 13 Mar 2018

Atmospheric water-soluble organic nitrogen (WSON) in the eastern Mediterranean: origin and ramifications regarding marine productivity

Münevver Nehir and Mustafa Koçak

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Final revised paper (published on 13 Mar 2018)
Preprint (discussion started on 24 Aug 2017)

Interactive discussion

Status: closed

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

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RC1: 'Review of Nehir and Koçak', Anonymous Referee #1, 25 Aug 2017
- AC1: 'Response to Reviewer 1', mustafa kocak, 05 Jan 2018
RC2: 'Review of the article entitled “Atmospheric Water-Soluble Organic Nitrogen (WSON) in the Eastern Mediterranean: Origin and Ramifications Regarding Marine Productivity” by Münevver Nehir and Mustafa Koçak.', Anonymous Referee #2, 28 Nov 2017
- AC2: 'Response to Reviewer 2', mustafa kocak, 05 Jan 2018

Peer-review completion

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

AR by Anna Wenzel on behalf of the Authors (09 Jan 2018) Author's response

ED: Publish as is (31 Jan 2018) by Evangelos Gerasopoulos

Short summary

Atmospheric samples of water-soluble organic nitrogen (WSON) obtained over the eastern Mediterranean have been investigated. Aerosol WSON concentrations exhibited large temporal variation, mainly due to rain and the origin of airflow. WSON originated from agricultural activities, secondary aerosol, nitrate, crustal material and sea salt. In the Cilician Basin, the WSON flux would sustain 33 % and 76 % of the new production of the plant-like organisms in coastal and open waters, respectively.