2006
DOI: 10.1109/tgrs.2005.863715
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Algorithm for NO/sub 2/ vertical column retrieval from the ozone monitoring instrument

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Cited by 281 publications
(282 citation statements)
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“…[7] The tropospheric NO 2 data utilized in this study are from the 0.25°× 0.25°gridded OMNO 2 L2G product, developed at NASA's Goddard Space Flight Center [Bucsela et al, 2006]. To retrieve NO 2 , spectral fitting in the OMI spectral range of 405-465 nm is used to derive the SCD of NO 2 , which is then converted to the NO 2 VCD with predetermined AMF's.…”
Section: Methodsmentioning
confidence: 99%
“…[7] The tropospheric NO 2 data utilized in this study are from the 0.25°× 0.25°gridded OMNO 2 L2G product, developed at NASA's Goddard Space Flight Center [Bucsela et al, 2006]. To retrieve NO 2 , spectral fitting in the OMI spectral range of 405-465 nm is used to derive the SCD of NO 2 , which is then converted to the NO 2 VCD with predetermined AMF's.…”
Section: Methodsmentioning
confidence: 99%
“…The nearreal-time OMI NO 2 product [Boersma et al, 2008b] was not available for 2005. Detailed descriptions of the algorithm for the standard OMI NO 2 data product are given in Boersma et al [2002], Bucsela et al [2006], . In brief, the standard algorithm uses the Differential Optical Absorption Spectroscopy (DOAS) technique [Platt, 1994] to determine the slant column densities by nonlinear least squares fitting in the 415 -465 nm window.…”
Section: Omi Tropospheric No 2 Columnsmentioning
confidence: 99%
“…In this study, NASA's OMI tropospheric NO 2 data product is used (Bucsela et al, 2006). The NO 2 slant column density (SCD) is retrieved by fitting the OMI spectrum for wavelengths ranging from 405 nm to 465 nm using the DOAS technique.…”
Section: Omi Tropospheric No 2 Vcd Retrievalmentioning
confidence: 99%
“…The AMF calculation depends on the viewing geometry, surface albedo, atmospheric scattering and the NO 2 vertical profile (Palmer et al, 2001). AMFs are calculated on the basis of annual mean NO 2 profiles obtained from the GEOSChem model ) and pre-calculated altitudedependent AMFs (Bucsela et al, 2006). The stratospheric and tropospheric amounts of NO 2 are separated by assuming the tropospheric NO 2 varies on a much smaller spatial scale than the stratospheric NO 2 .…”
Section: Omi Tropospheric No 2 Vcd Retrievalmentioning
confidence: 99%
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