2008
DOI: 10.1029/2007jd008808
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The 2005 and 2006 DANDELIONS NO2 and aerosol intercomparison campaigns

Abstract: Environment (RIVM) NO 2 lidar. We show that NO 2 from Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) compares well with in situ measurements. We show that different MAX-DOAS instruments, operating simultaneously during the campaign, give very similar results. We also provide unique information on the spatial homogeneity and the vertical and temporal variability of NO 2 , showing that during a number of days, the NO 2 columns derived from measurements in different directions varied significa… Show more

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Cited by 136 publications
(171 citation statements)
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References 34 publications
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“…The slope of the correlations was found to be 0.69 ± 0.04, indicating a negative bias in the OMI data by 31 ± 4%. This is consistent with other validation studies (e.g., Celarier et al 2008). After the estimated bias was taken into account, the mean trend over the industrial area of China (30° 40°N and 110° 123°E) was estimated to be about 5 ± 3% per year ((7 ± 5) × 10 14 molecules cm 2 per year) for 2005 2008.…”
Section: Discussionsupporting
confidence: 90%
See 1 more Smart Citation
“…The slope of the correlations was found to be 0.69 ± 0.04, indicating a negative bias in the OMI data by 31 ± 4%. This is consistent with other validation studies (e.g., Celarier et al 2008). After the estimated bias was taken into account, the mean trend over the industrial area of China (30° 40°N and 110° 123°E) was estimated to be about 5 ± 3% per year ((7 ± 5) × 10 14 molecules cm 2 per year) for 2005 2008.…”
Section: Discussionsupporting
confidence: 90%
“…The correlation coefficient for the regression analysis (R 2 ) is as high as 0.64, indicating that the relative changes seen in OMI data are very accurate. The regression line has a slope of 0.69 ± 0.04, indicating a negative bias of 31 ± 4% on average in the OMI data analyzed here, consistent with other validation comparisons, which suggested a negative bias of about 15 30% (e.g., Celarier et al 2008).…”
Section: Omisupporting
confidence: 90%
“…For each scan, VCD a is derived using the geometrical approximation method; that is, the SO 2 layer is assumed to be located below the scattering altitude at 30 • EVA, so that tropospheric SO 2 VCDs can be derived by applying a geometrical air mass factor (AMF) to measured 30 • EVA DSCDs (Hönninger et al, 2004;Brinksma et al, 2008; see also Hendrick et al, 2014). In case of aerosols, a fixed AOD of 0.2 is used.…”
Section: Atmosmentioning
confidence: 99%
“…2). This location was chosen because of its unobstructed views close to horizontal at many azimuth angles, its large variability in tropospheric NO 2 , the absence of local pollution sources, good local support because of its closeness to KNMI headquarters in De Bilt near Utrecht, and its tower of height over 200 m. The same site has been used for two previous MAX-DOAS campaigns focusing on validation of satellite observations (Brinksma et al, 2008;Hains et al, 2010). The Cabauw site has a large suite of meteorological instruments deployed continuously, specialising in the boundary layer.…”
Section: The Intercomparison Campaignmentioning
confidence: 99%