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Simultaneous Measurements of Black Carbon, PM10, Ozone and NOx Variability at a Locally Polluted Island in the Southern Tropics
Authors:Chatrapatty Bhugwant  Philippe Brémaud
Affiliation:(1) Laboratoire de Physique de l'Atmosphère, Université de la Réunion, B.P. 7151-15 Avenue René Cassin, 97715 Saint-Denis Messag Cedex 9, La Réunion island, France;(2) Lycée d'Einseignement Général et Technologique, Voie Romaine, 63400 Chamalières, France
Abstract:This paper shows a comparative study of particle and surface ozone concentration measurements undertaken simultaneously at two distinct semi-urban locations distant by 4 km at Saint-Denis, the main city of La Réunion island (21.5° S, 55.5° E) during austral autumn (May 2000). Black carbon (BC) particles measured at La Réunion University, the first site situated in the suburbs of Saint-Denis, show straight-forward anti-correlation with ozone, especially during pollution peaks (sim 650 ng/m3 and 15 ppbv, for BC and ozone respectively) and at night-time (sim90 ng/m3 and 18.5 ppbv, for BC and ozone respectively). NOx (NO and NO2) and PM10 particles were also measured in parallel with ozone at Lislet Geoffroy college, a second site situated closer to the city centre. NOx and PM10 particles are anti-correlated with ozone, with noticeable ozone destruction during peak hours (mean sim6 and 9 ppbv at 7 a.m. and 8 p.m. respectively) when NOx and PM10 concentrations exhibit maximum values. We observe a net daytime ozone creation (sim19 ppbv, DeltaO3 sim +4.5 ppbv), following both photochemical and dynamical processes. At night-time however, ozone recovers (mean sim11 ppbv) when anthropogenic activities are lower (BC] sim100 ng/m3). BC and PM10 concentration variation obtained during an experiment at the second site shows that the main origin of particles is anthropogenic emission (vehicles), which in turn influences directly ozone variability. Saint-Denis BC and ozone concentrations are also compared to measurements obtained during early autumn (March 2000) at Sainte-Rose (third site), a quite remote oceanic location. Contrarily to Saint-Denis observations, a net daytime ozone loss (sim14.5 ppbv at 4 p.m.) is noticed at Sainte-Rose while ozone recovers (sim17 ppbv) at night-time, with however a lower amplitude than at Saint-Denis. Preliminary results presented here are handful data sets for modelling and which may contribute to a better comprehension of ozone variability in relatively polluted areas.
Keywords:black carbon  PM10  ozone  NOx  tropical  marine  pollutants  boundary layer
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