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Seasonal dependence of peroxy radical concentrations at a Northern hemisphere marine boundary layer site during summer and winter: evidence for radical activity in winter

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Fig. 1. Location of Weybourne Atmospheric Observatory, Norfolk, UK (adapted from Cardenas et al., 1998).
Fig. 2. The variation of the derived water correction factor, applied to HO 2 + 6RO 2 PERCA data, with specific humidity and temperature (after Salisbury et al., 2002).
Figure 3 shows histograms of all the hourly wind direc- direc-tions reaching Weybourne during the winter and summer campaigns
Fig. 5. Campaign profiles of (HO 2 + 6RO 2 ), j(O 1 D) and NO and NO 2 (hourly averaged data).
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