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<p><strong>Abstract.</strong> Nitric oxide (NO) is a short–lived intermediate of the oceanic nitrogen cycle. However, our knowledge about its production and consumption pathways in oceanic environments is rudimentary. In order to decipher the major factors affecting NO photochemical production, we irradiated artificial seawater samples as well as natural surface seawater samples in laboratory experiments. The seawater samples were collected during a cruise to the western tropical North Pacificdoi:10.5194/os-2019-57 fatcat:6b3v55qearfchmyyrxw5gwmbmy