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Variation in ozone concentration in relation to local climate in south-west Sweden

Sundberg, Jenny, 1978 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences,Göteborg University
Karlsson, Per Erik, 1957 (författare)
Göteborg University
Schenk, Linda, 1980- (författare)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences
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Pleijel, Håkan, 1958 (författare)
Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences,Göteborg University
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 (creator_code:org_t)
2006-05-03
2006
Engelska.
Ingår i: Water Air and Soil Pollution. - : Springer Science and Business Media LLC. - 0049-6979 .- 1573-2932. ; 173:1-4, s. 339-354
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Ozone (O-3) concentration and air temperature/relative humidity were monitored using diffusive samplers (weekly, 3 m above ground) and Tinytag loggers (10 min sampling, 1 m above ground, self-ventilating radiation shields), respectively, in the forested landscape of south-west Sweden, 40 km north-east of Gothenburg. Two forest sites were included, one at a hilltop (175 m a.s.l.), and one in a nearby (similar to 1 km) valley (110 m a.s.l.). In addition, a valley site (similar to 3 km from the forest sites, 60 m a.s.l.) in an agricultural landscape was included, where ozone was measured using both a UV-based monitor and diffusive sampling. At the agricultural site measurements of temperature and relative humidity were made using a radiation shield with forced ventilation and with Tinytags, as on the forest sites, in addition to observations of wind speed and the vertical temperature gradient. Furthermore, comparison with O-3 concentrations at urban and coastal sites in the region was made. The temperature dependent, systematic error of using a self-ventilating radiation shield was estimated and corrected for. It was found that the elevated forested site experienced higher O-3 concentrations and lower evening cooling rates in calm situations as compared to the forest site in the valley and in particular as compared to the agricultural site. This can be explained by a stronger coupling with the planetary boundary layer at the elevated site and more pronounced night-inversions at the valley sites. The difference in weekly O-3 concentration between the two forested sites was correlated with the difference in average minimum night-time temperature. The coastal site had the highest ozone concentrations, related largely, but not fully, to higher night-time O-3 concentrations. The urban site showed a depression in O-3 concentration associated with the combination of large NO emissions and slow air mixing during the morning traffic rush hours.

Ämnesord

NATURVETENSKAP  -- Biologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)

Nyckelord

coast
cooling rate
heat island
inland
inversion
local climate
ozone
topoclimatology
SPATIAL-DISTRIBUTION
COMPLEX TERRAIN
NO2
O-3

Publikations- och innehållstyp

ref (ämneskategori)
art (ämneskategori)

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