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Ground Based Gas Phase Measurements in Surinam during the LBA-Claire 98 Experiment
Authors:J Quesada  D Grossmann  E Fernández  J Romero  E Sanhueza  G Moortgat  P J Crutzen
Institution:(1) MPI für Chemie, Luftchemie, Postfach 3060, 55020 Mainz, Germany;(2) IVIC, Atmospheric Chemistry Laboratory, Apartado 21827, Caracas, 1020A, Venezuela;(3) MPI für Chemie, Luftchemie, Postfach 3060, 55020 Mainz, Germany
Abstract:As part of the LBA-CLAIRE-98 experiment, ground level atmosphericconcentrations of O3, CO, hydroperoxides and organic acids weremeasured in the rainforest region in Surinam. Measurements of CO andO3 were also made at a coastal site.The results suggest that a significant consumption of `boundary layer' ozoneoccurs over the forested region of Surinam, with an estimated net ozoneconsumption of about 5% hr–1 during daytime. Thiswould be mainly explained by a low photochemical production and high drydeposition to the forest vegetation. Compared to other tropical sites, lowerlevels of H2O2 were observed at the rainforest site,with an average boundary layer concentration of 0.55± 0.2 nmolmol–1. Also acetic and formic acids showed relatively lowaverage boundary layer mixing ratios; 1.1± 0.4 nmolmol–1 and 1.4± 0.5 nmol mol–1,respectively. Significant correlations were found between both acids andbetween the acids and hydrogen peroxide, suggesting an atmospheric source forthe acids.From the available observations we discuss possible implications of ourmeasurements for the O3, HO2, and NOx budgetsand concentrations in the boundary layer. We conclude that, despite the highsolar irradiation, relatively low levels of O3,H2O2, HCOOH and CH3COOH are observed in theboundary layer of the rainforest of Surinam, probably due to low levels ofNOx and high levels of VOCs, which leads to loss of OH andHO2 radicals. Additionally, high deposition rates of these gasesoccur to the forest vegetation.
Keywords:LBA-Claire  atmospheric tropical photochemistry  tropical forest  ozone  hydrogenperoxide  gaseous organic acids
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