Band residual difference algorithm for retrieval of SO/sub 2/ from the aura ozone monitoring instrument (OMI)

By N. Krotkov, S. Carn, A. Krueger, Pawan K. Bhartia, Kai Yang. IEEE Transactions on Geoscience and Remote Sensing, 2006

299 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/c60192936b5b4a2e22e9ccb74387457c1ddc977b

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Citations in the corpus

Science objectives of the ozone monitoring instrument (2006, methodology): “For further details on the OMI SO product see [21].”
Observations of the eruption of the Sarychev volcano and simulations using the HadGEM2 climate model. (2010, methodology): “While SO2 detection has been possible using the Ozone Monitoring Instrument (OMI) [e.g., Krotkov et al., 2006; Prataetal.,2007;Yangetal.,2007]andIASI[Clarisseetal., 2008, 2010] detection of stratospheric aerosols from low VEI eruptions is more challenging to detect from space owing to the low stra”
Cleaning up the air: effectiveness of air quality policy for SO 2 and NO x emissions in China (2016, background): “(2008), Kurokawa et al. (2009), and more recently by Mijling et al.”
Estimation of the vertical profile of sulfur dioxide injection into the atmosphere by a volcanic eruption using satellite column measurements and inverse transport modeling (2008, methodology): “The retrieval schemes used to determine column SO2 are described by Krotkov et al. (2006) and Yang et al. (2007) while use of OMI SO2 data in volcanological applications can be found in the papers by Carn et al. (2007a) and Carn et al. (2007b).”
Observational evidence of aerosol enhancement of lightning activity and convective invigoration (2011, background): “SO2 (precursor for sulfate aerosol) column amounts [ Krotkov et al., 2006 ] come from the Ozone Monitoring Instrument (OMI) onboard the Aura satellite.”
Retrieval of large volcanic SO2 columns from the Aura Ozone Monitoring Instrument: Comparison and limitations (2007, methodology): “In the BRD algorithm, the OMTO3 residuals are corrected by subtracting its corresponding orbital equatorial averages, calculated after excluding heavily SO2 contaminated pixels [Krotkov et al., 2006].”
A fast and sensitive new satellite SO2 retrieval algorithm based on principal component analysis: Application to the ozone monitoring instrument (2013, methodology): “The operational OMI level-2 (L2) planetary boundary layer (PBL) SO2 data are produced using the Band Residual Difference (BRD) method that utilizes three selected wavelength pairs to maximize sensitivity to PBL pollution [Krotkov et al., 2006].”