2023
DOI: 10.1016/j.scitotenv.2022.160895
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Seasonal source identification and formation processes of marine particulate water soluble organic nitrogen over an offshore island in the East China Sea

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Cited by 6 publications
(10 citation statements)
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“…Figure 6c shows that the HCHO value of ZS began to decline in the morning and increased from 14:00 to 18:00. This may relate to changes in wind speed and direction in the island region [26,27]. The HCHO value of the NJ site increased from 10:00 to approximately 14:00, remained constant until 17:00, and then began to decline.…”
Section: Diurnal and Weekly Variations Of Aerosols No2 And Hchomentioning
confidence: 96%
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“…Figure 6c shows that the HCHO value of ZS began to decline in the morning and increased from 14:00 to 18:00. This may relate to changes in wind speed and direction in the island region [26,27]. The HCHO value of the NJ site increased from 10:00 to approximately 14:00, remained constant until 17:00, and then began to decline.…”
Section: Diurnal and Weekly Variations Of Aerosols No2 And Hchomentioning
confidence: 96%
“…The AE peak of the NJ site appeared in the afternoon. Figure 6b shows that the variation in NO2 during the daytime is not apparent at ZS, mainly due to the low traffic emissions, and there was no obvious traffic emission source [27]. In addition, the photolysis of NO2 led to the low NO2 value near noon [8].…”
Section: Diurnal and Weekly Variations Of Aerosols No2 And Hchomentioning
confidence: 98%
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