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Sökning: WFRF:(Reis D. A.) > (2010-2014) > Modelling surface o...

Modelling surface ozone during the 2003 heat-wave in the UK

Vieno, M. (författare)
University of Edinburgh,UK Centre For Ecology & Hydrology (UKCEH)
Dore, A. J. (författare)
UK Centre For Ecology & Hydrology (UKCEH)
Stevenson, D. S. (författare)
University of Edinburgh
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Doherty, R. (författare)
University of Edinburgh
Heal, M. R. (författare)
University of Edinburgh
Reis, S. (författare)
UK Centre For Ecology & Hydrology (UKCEH)
Hallsworth, S. (författare)
UK Centre For Ecology & Hydrology (UKCEH)
Tarrason, L. (författare)
Norsk institutt for luftforskning (NILU),Norwegian Institute for Air Research (NILU)
Wind, P. (författare)
Meteorologisk institutt,Norwegian Meteorological Institute
Fowler, D. (författare)
UK Centre For Ecology & Hydrology (UKCEH)
Simpson, David, 1961 (författare)
Chalmers tekniska högskola,Chalmers University of Technology
Sutton, M. A. (författare)
UK Centre For Ecology & Hydrology (UKCEH)
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 (creator_code:org_t)
2010-08-27
2010
Engelska.
Ingår i: Atmospheric Chemistry and Physics. - : Copernicus GmbH. - 1680-7316 .- 1680-7324. ; 10:16, s. 7963-7978
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
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  • The EMEP4UK modelling system is a high resolution (5x5 km(2)) application of the EMEP chemistry-transport model, designed for scientific and policy studies in the UK. We demonstrate the use and performance of the EMEP4UK system through the study of ground-level ozone (O-3) during the extreme August 2003 heat-wave. Meteorology is generated by the Weather Research and Forecast (WRF) model, nudged every six hours with reanalysis data. We focus on SE England, where hourly average O-3 reached up to 140 ppb during the heat-wave. EMEP4UK accurately reproduces elevated O-3 and much of its day-to-day variability during the heat-wave. Key O-3 precursors, nitrogen dioxide and isoprene, are less well simulated, but show generally accurate diurnal cycles and concentrations to within a factor of similar to 2-3 of observations. The modelled surface O-3 distribution has an intricate spatio-temporal structure, governed by a combination of meteorology, emissions and photochemistry. A series of sensitivity runs with the model are used to explore the factors that influenced O-3 levels during the heat-wave. Various factors appear to be important on different days and at different sites. Ozone imported from outside the model domain, especially the south, is very important on several days during the heat-wave, contributing up to 85 ppb. The effect of dry deposition is also important on several days. Modelled isoprene concentrations are generally best simulated if isoprene emissions are changed from the base emissions: typically doubled, but elevated by up to a factor of five on one hot day. We found that accurate modelling of the exact positions of nitrogen oxide and volatile organic compound plumes is crucial for the successful simulation of O-3 at a particular time and location. Variations in temperature of +/- 5 K were found to have impacts on O-3 of typically less than +/- 10 ppb.

Ämnesord

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

Nyckelord

europe
sensitivity
photochemical
deposition
organic-compound emissions
inventory
milan area i
air-pollution
isoprene
biogenic emissions
ozone

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