Journal of Geophysical Research Atmospheres · 2012 · 148 citations · 55 references
Natural SciencesChemistryEarth SciencesAtmospheric ChemistryAtmospheric ScienceEnvironmental ChemistryAir MassesAir PollutantsAir Pollution ChemistryAir QualityAtmospheric Radical ChemistryVolatile Organic CompoundsAir Mass MixingAir Mass VariabilityChemical Master EquationDaytime Radical ChemistryMeasurementMeasurement TechniquesModel Intercomparison StudiesRadical Budget Analysis
Recent studies have shown that measured OH under NO x ‐limited, high‐isoprene conditions are many times higher than modeled OH. In this study, a detailed analysis of the HO x radical budgets under low‐NO x , rural conditions was performed employing a box model based on the Master Chemical Mechanism (MCMv3.2). The model results were compared with HO x radical measurements performed during the international HOxComp campaign carried out in Jülich, Germany, during summer 2005. Two different air masses influenced the measurement site denoted as high‐NO x (NO, 1–3 ppbv) and low‐NO x (NO, < 1 ppbv) periods. Both modeled OH and HO 2 diurnal profiles lay within the measurement range of all HO x measurement techniques, with correlation slopes between measured and modeled OH and HO 2 around unity. Recently discovered interference in HO 2 measurements caused by RO 2 cross sensitivity was found to cause a 30% increase in measured HO 2 during daytime on average. After correction of the measured HO 2 data, the model HO 2 is still in good agreement with the observations at high NO x but overpredicts HO 2 by a factor of 1.3 to 1.8 at low NO x . In addition, for two different set of measurements, a missing OH source of 3.6 ± 1.6 and 4.9 ± 2.2 ppb h −1 was estimated from the experimental OH budget during the low‐NO x period using the corrected HO 2 data. The measured diurnal profile of the HO 2 /OH ratio, calculated using the corrected HO 2 , is well reproduced by the MCM at high NO x but is significantly overestimated at low NO x . Thus, the cycling between OH and HO 2 is better described by the model at high NO x than at low NO x . Therefore, similar comprehensive field measurements accompanied by model studies are urgently needed to investigate HO x recycling under low‐NO x conditions.
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