Articles | Volume 16, issue 1
Ocean Sci., 16, 135–148, 2020
https://doi.org/10.5194/os-16-135-2020
Ocean Sci., 16, 135–148, 2020
https://doi.org/10.5194/os-16-135-2020

Research article 23 Jan 2020

Research article | 23 Jan 2020

Photoproduction of nitric oxide in seawater

Ye Tian et al.

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Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Chun-ying Liu on behalf of the Authors (16 Sep 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (24 Sep 2019) by Mario Hoppema
RR by Anonymous Referee #1 (15 Nov 2019)
ED: Publish subject to minor revisions (review by editor) (26 Nov 2019) by Mario Hoppema
AR by Chun-ying Liu on behalf of the Authors (05 Dec 2019)  Author's response    Manuscript
ED: Publish as is (13 Dec 2019) by Mario Hoppema
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Short summary
Nitric oxide (NO) could be produced by nitrite photolysis; the rates from dissolved nitrite in artificial seawater showed increasing trends with decreasing pH, increasing temperatures, and increasing salinity. However, NO photoproduction from the natural seawater samples did not show correlations with pH, water temperature, salinity, or dissolved nitrite concentrations in the western tropical North Pacific Ocean (WNTP). And there were other NO loss processes in the surface layer of WNTP.