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2013
DOI: 10.5194/amtd-6-1361-2013
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A new stratospheric and tropospheric NO<sub>2</sub> retrieval algorithm for nadir-viewing satellite instruments: applications to OMI

Abstract: We describe a new algorithm for the retrieval of nitrogen dioxide (NO2) vertical columns from nadir-viewing satellite instruments. This algorithm (SP2) is the basis for the Version 2.1 OMI NO2 Standard Product and features a novel method for separating the stratospheric and tropospheric columns. The approach estimates the stratospheric NO2 directly from satellite data without using stratospheric chemical transport models or assuming any global zonal wave pattern. Tropospheric N… Show more

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Cited by 58 publications
(92 citation statements)
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“…Differential Optical Absorption Spectroscopy (DOAS) [3], which is a method to retrieve total amounts of atmospheric trace gases through the remote sensing measurement of light in the ultra violet, visible, and near infrared spectral range, is widely used to monitor NO 2 using both ground-based remote sensing measurements, such as Multi-Axis DOAS, and space-born instruments such as the Global Ozone Monitoring Experiment (GOME) [4], the Scanning Imaging Spectrometer for Atmospheric Cartography (SCIAMACHY), the Ozone Monitoring Instrument (OMI) [5,6], and GOME-2 [2,7]. The key idea of the DOAS method is to separate broad and narrow band spectral structures of the absorption spectra in order to find the narrow trace gas absorption features.…”
Section: Introductionmentioning
confidence: 99%
“…Differential Optical Absorption Spectroscopy (DOAS) [3], which is a method to retrieve total amounts of atmospheric trace gases through the remote sensing measurement of light in the ultra violet, visible, and near infrared spectral range, is widely used to monitor NO 2 using both ground-based remote sensing measurements, such as Multi-Axis DOAS, and space-born instruments such as the Global Ozone Monitoring Experiment (GOME) [4], the Scanning Imaging Spectrometer for Atmospheric Cartography (SCIAMACHY), the Ozone Monitoring Instrument (OMI) [5,6], and GOME-2 [2,7]. The key idea of the DOAS method is to separate broad and narrow band spectral structures of the absorption spectra in order to find the narrow trace gas absorption features.…”
Section: Introductionmentioning
confidence: 99%
“…In the normal global operational mode, the OMI ground pixel at nadir is 13 km × 24 km, with a local equator-crossing time of 13:45 h in ascending node. The OMI NO 2 data are filtered using quality flags, cloudiness, and row anomaly (an anomaly caused by an obstruction in part of OMI's aperture) [Bucsela et al, 2013]. Additionally, we apply a cutoff value (0.7 × 10 15 molecules cm À2 ) to the OMI data as low-value pixels are less responsive to local emission density but more influenced by regional background and retrieval noise.…”
Section: Methodsmentioning
confidence: 99%
“…These morning hours are associated with the highest NO x concentrations contributed by both typical commuter traffic peaks and the shallow planetary boundary layer, making them an ideal indicator for assessing local emission conditions [Tong et al, 2015]. Besides ground data, the OMI standard product (version 2.1, collection 3) described by Bucsela et al [2013] is used to derive the satellite-based emission trends using the data-filtering approach described in Tong et al [2015]. In the normal global operational mode, the OMI ground pixel at nadir is 13 km × 24 km, with a local equator-crossing time of 13:45 h in ascending node.…”
Section: Methodsmentioning
confidence: 99%
“…The DOAS method is also applied to assess total and tropospheric NO 2 columns from nadir-viewing spaceborne sensors like SCIAMACHY (scanning imaging absorption chartography), GOME (Global Ozone Monitoring Experiment), GOME-2, and OMI (Ozone Monitoring Experiment) (see e.g. Richter and Burrows, 2002;Beirle et al, 2010;Boersma et al, 2011;Valks et al, 2011;Bucsela et al, 2013;Hilboll et al, 2013). Other experiments have been published, presenting approaches to monitor tropospheric NO 2 from car (Johansson et al, 2009;Wagner et al, 2010;Constantin et al, 2013) and airborne platforms (Berg et al, 2012;Popp et al, 2012).…”
Section: Introductionmentioning
confidence: 99%