WFRF:(Pihl Karlsson G.)
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- Pleijel, Håkan,1958Gothenburg University,Göteborgs universitet,Institutionen för biologi och miljövetenskap,Department of Biological and Environmental Sciences (författare)
Surface Ozone in the Marine Environment—Horizontal Ozone Concentration Gradients in Coastal Areas
- Artikel/kapitelEngelska2013
Förlag, utgivningsår, omfång ...
- 2013-06-09
- Springer Science and Business Media LLC,2013
Nummerbeteckningar
- LIBRIS-ID:oai:gup.ub.gu.se/178849
- https://gup.ub.gu.se/publication/178849URI
- https://doi.org/10.1007/s11270-013-1603-4DOI
Kompletterande språkuppgifter
- Språk:engelska
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- SwePubSwePub
Klassifikation
Anmärkningar
- Spring/summer surface ozone concentrations, [O3], in coastal environments were investigated: (1) by comparison of coastal and inland monitoring stations with data from a small island >5 km off the coast of southwest Sweden, (2) as a gradient from the coast towards inland in southernmost Sweden. Further, results from the chemical transport model MATCH were used to assess the marine influence on [O3]. It was hypothesised that [O3] is higher on the small island compared to the coast, especially during night and in offshore wind. Another hypothesis was that [O3] declines from the coast towards inland. Our hypotheses were based on observations that the deposition velocity of O3 to sea surfaces is lower than to terrestrial surfaces, and that vertical air mixing is stronger in the marine environment, especially during night. The island experienced 10 % higher [O3] compared to the coast. This difference was larger with offshore (15 %) than onshore wind (9 %). The concentration difference between island and coast was larger during night, but prevailed during day and could not be explained by differences in [NO2] between the sites. The difference in [O3] between the island and the inland site was 20 %. Higher [O3] over the sea, especially during night, was reproduced by MATCH. In the gradient study, [O3] declined from the coast towards inland. Both [O3] and [NO2] were elevated at the coast, indicating that the gradient in [O3] from the coast was not caused by NO titration. The conclusions were that surface [O3] in marine environments is higher than in coastal, and higher in coastal than inland areas, especially during night.
Ämnesord och genrebeteckningar
- NATURVETENSKAP Geovetenskap och miljövetenskap Meteorologi och atmosfärforskning hsv//swe
- NATURAL SCIENCES Earth and Related Environmental Sciences Meteorology and Atmospheric Sciences hsv//eng
- NATURVETENSKAP Geovetenskap och miljövetenskap Miljövetenskap hsv//swe
- NATURAL SCIENCES Earth and Related Environmental Sciences Environmental Sciences hsv//eng
- NATURVETENSKAP Geovetenskap och miljövetenskap hsv//swe
- NATURAL SCIENCES Earth and Related Environmental Sciences hsv//eng
- Ozone
- Wind direction
- Coast
- Marine boundary layer
- Terrestrial boundary layer
- Nitrogen dioxide
Biuppslag (personer, institutioner, konferenser, titlar ...)
- Klingberg, Jenny,1978Gothenburg University,Göteborgs universitet,Institutionen för biologi och miljövetenskap,Department of Biological and Environmental Sciences(Swepub:gu)xsundj (författare)
- Pihl Karlsson, G. (författare)
- Engardt, Magnuz (författare)
- Karlsson, Per Erik (författare)
- Göteborgs universitetInstitutionen för biologi och miljövetenskap (creator_code:org_t)
Sammanhörande titlar
- Ingår i:Water, Air and Soil Pollution: Springer Science and Business Media LLC224:70049-69791573-2932
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- Water, Air and Soil Pollution (Sök värdpublikationen i LIBRIS)
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