2006
DOI: 10.1007/s10874-006-9049-3
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Intercomparison of Two Hydroxyl Radical Measurement Techniques at the Atmosphere Simulation Chamber SAPHIR

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Cited by 84 publications
(98 citation statements)
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“…One air spectrum is recorded within 135 s. A comparison of measured and modelled MCST spectra is given by Hausmann et al (1997) who found a maximum 1.7% error contribution to the accuracy of the measurement. The deconvolution of the measured spectrum is performed by fitting a trigonometric background consisting of 16 terms and three reference spectra, namely OH, HCHO, and an so far unidentified absorber X (Schlosser et al, 2006). We present the HCHO data in units of the optical density (absorbance) at 308.1034 nm (see Fig.…”
Section: High-resolution Doas Instrumentmentioning
confidence: 99%
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“…One air spectrum is recorded within 135 s. A comparison of measured and modelled MCST spectra is given by Hausmann et al (1997) who found a maximum 1.7% error contribution to the accuracy of the measurement. The deconvolution of the measured spectrum is performed by fitting a trigonometric background consisting of 16 terms and three reference spectra, namely OH, HCHO, and an so far unidentified absorber X (Schlosser et al, 2006). We present the HCHO data in units of the optical density (absorbance) at 308.1034 nm (see Fig.…”
Section: High-resolution Doas Instrumentmentioning
confidence: 99%
“…Multiple reflection cells, however, allow the setup of DOAS measurements with long light paths inside simulation chambers of different sizes (e.g. De Haan et al, 1999;Kleffmann et al, 2006;Schlosser et al, 2006;Bossmeyer, 2006).…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…From these measurements, concentrations of HO 2 and RO 2 radicals were determined. Moreover, differential optical absorption spectroscopy (DOAS) (Dorn et al, 1995;Schlosser et al, 2007Schlosser et al, , 2009) was employed for the measurement of OH radical concentrations.…”
Section: Analytical Instrumentationmentioning
confidence: 99%
“…It provides a large volume of homogeneously mixed air, to which trace gases can be added at tropospheric concentration levels. For instrumental comparisons, it ensures that the instruments sample air of the same composition and at natural conditions, as was demonstrated for OH (Schlosser et al, 2007) and oxygenated volatile organic compounds (Apel et al, 2008). A further advantage of the use of a chamber is that experiments can be carried out at controlled conditions, allowing, for example, to keep radical concentrations constant at different levels.…”
Section: Introductionmentioning
confidence: 99%