Error analysis for tropospheric NO2 retrieval from space

By K. F. Boersma, H. Eskes, E. Brinksma. 2004

762 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/d01f7b0b3f885c4f37af204e83fa2018e95477aa

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Citations in the corpus

Evaluation of space‐based constraints on global nitrogen oxide emissions with regional aircraft measurements over and downwind of eastern North America (2006, background): “[2002b, 2003b] and Boersma et al. [2004] estimated that the total uncertainty in the GOME retrieval of tropospheric NO2 columns over continental source regions is largely determined by the AMF calculation due primarily to surface reflectivity, clouds, aerosols, and the trace gas profile.”
Multi-model ensemble simulations of tropospheric NO2 compared with GOME retrievals for the year 2000 (2006, neutral): “Reference Boersma et al. (2004) Richter et al. (2005) Martin et al. (2003b); the version used in this study is the release of May 2005, which uses an improved fitting algorithm”
Effective cloud fractions from the Ozone Monitoring Instrument: Theoretical framework and validation (2008, background): “Errors in these cloud products will directly end up in errors in ozone [Vasilkov et al., 2004; Joiner et al., 2006] and NO2 [Boersma et al., 2004].”
Science objectives of the ozone monitoring instrument (2006, background): “In Fig. 4 first preliminary tropospheric NO retrievals are shown above Australia, based on the assumption that stratospheric NO data are generally zonal [ 18 ], [19].”
Remote sensed and in situ constraints on processes affecting tropical tropospheric ozone (2006, methodology): “Variability in the stratospheric NO 2 columns is accounted for using assimilated stratospheric NO 2 columns from Boersma et al. (2004), a minor issue in the Tropics. Martin et al. (2004) evaluated the GOME retrieval with airborne in situ measurements of NO 2 and HCHO over the Southeastern United Sta”
Retrieving tropospheric nitrogen dioxide from the Ozone Monitoring Instrument: effects of aerosols, surface reflectance anisotropy, and vertical profile of nitrogen dioxide (2013, methodology): “Rather, these retrievals assume that the cloud correction accounts for the effect of aerosols, as the OMI cloud retrieval provides effective cloud parameters sensitive to aerosol burdens (Boersma et al., 2011).”