2019
DOI: 10.5194/amt-12-3365-2019
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The ICAD (iterative cavity-enhanced DOAS) method

Abstract: Abstract. Cavity-enhanced differential optical absorption spectroscopy (CE-DOAS or BB-CEAS DOAS) allows us to make in situ measurements while maintaining the kilometre-long light paths required by DOAS. This technique has been successfully used for several years to measure in situ atmospheric trace gases. A property of optical cavities is that in the presence of strong absorbers or scatterers the light path is reduced, in contrast to classical long-path DOAS measurements where the light path is fixed. Typical … Show more

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Cited by 24 publications
(18 citation statements)
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“…In former publications (e.g. Irie et al, 2008;Clémer et al, 2010;Frieß et al, 2016;Bösch et al, 2018) and also during this comparison study, it was found that MAX-DOAS vertically integrated aerosol profiles systematically underestimate AOTs. It has already been pro-J.-L. Tirpitz et al: CINDI-2 profiling comparison Figure 10.…”
Section: Aerosol Optical Thicknesssupporting
confidence: 65%
See 1 more Smart Citation
“…In former publications (e.g. Irie et al, 2008;Clémer et al, 2010;Frieß et al, 2016;Bösch et al, 2018) and also during this comparison study, it was found that MAX-DOAS vertically integrated aerosol profiles systematically underestimate AOTs. It has already been pro-J.-L. Tirpitz et al: CINDI-2 profiling comparison Figure 10.…”
Section: Aerosol Optical Thicknesssupporting
confidence: 65%
“…Multi-axis differential optical absorption spectroscopy (MAX-DOAS) (e.g. Hönninger and Platt, 2002;Hönninger et al, 2004;Wagner et al, 2004;Heckel et al, 2005;Frieß et al, 2006;Platt and Stutz, 2008;Irie et al, 2008;Clémer et al, 2010;Wagner et al, 2011;Vlemmix et al, 2015b) is a widely used ground-based measurement technique for the detection of aerosols and trace gases particularly in the lower troposphere: ultraviolet (UV) and visible (Vis) absorption spectra of skylight are analysed to obtain information on different atmospheric absorbers and scatterers, integrated over the light path (in fact, a superposition of a multitude of light paths). The amount of atmospheric trace gases along the light path is inferred by identifying and analysing their characteristic narrow spectral absorption features, applying DOAS (Platt and Stutz, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…5 minutes). Further, a CAPS (type AS32M, based on attenuated phase shift spectroscopy, Kebabian et al, 2005) and a CE-DOAS (cavity enhanced DOAS, Platt et al, 2009 andHorbanski et al, 2019) were continuously measuring at 27 m altitude. All the in situ measurements at the tower were combined to obtain another set of surface concentration measurements, more representative for concentrations close to the site.…”
Section: Trace Gas Surface Concentrationsmentioning
confidence: 99%
“…Since the first application of IBBCEAS by Fiedler (Fiedler et al, 2003), it has been widely used in laboratory studies and field campaigns to measure atmospheric trace gases such as H 2 O, O 3 , O 4 , IO, I 2 , OIO, SO 2 , NO 2 , NO 3 , N 2 O 5 , HONO, HCHO, GLY, and MGLY (Vaughan et al, 2008;Washenfelder et al, 2008;Thalman and Volkamer, 2010;Axson et al, 2011;Kahan et al, 2012;Min et al, 2016;Duan et al, 2018). The core part of the instrument is a high-finesse cavity that holds of a pair of highreflectivity mirrors, which typically have reflectivity greater than 0.9999.…”
Section: Glyoxalmentioning
confidence: 99%