Retrieval of large volcanic SO2 columns from the Aura Ozone Monitoring Instrument: Comparison and limitations
By Kai Yang, N. Krotkov, A. Krueger, S. Carn, Pawan K. Bhartia, Pieternel F. Levelt. 2007
215 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/14e4b4bf0e526e0cb6985e102a1914a791085b75
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In Atmospheric Science
- P. Seibert
- S. Eckhardt
- J. Haywood
- Andreas Stohl
- Alfredo J. Prata
- Kerstin Stebel
- N. Bellouin
- I. Pisso
In Global and Planetary Change
- Andreas Stohl
- P. Seibert
- S. Eckhardt
- J. Haywood
- Alfredo J. Prata
- Kerstin Stebel
- N. Bellouin
- I. Pisso
Citations in the corpus
- Tracking and quantifying volcanic SO 2 with IASI, the September 2007 eruption at Jebel at Tair (2008, methodology): “Imaging Absorption Spectrometer for Atmospheric CartograpHY (SCIAMACHY, e.g. Lee et al., 2008) and Ozone Monitoring Instrument (OMI, e.g.Yang et al., 2007).”
- Observations of the eruption of the Sarychev volcano and simulations using the HadGEM2 climate model. (2010, methodology): “While SO 2 detection has been possible using the Ozone Monitoring Instrument (OMI) [e.g., Krotkov et al. , 2006; Prata et al. , 2007; Yang et al. , 2007] and IASI [ Clarisse et al. , 2008, 2010] detection of stratospheric aerosols from low VEI eruptions is more challenging to detect from space…”
- 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).”
- Retrieval of sulphur dioxide from the infrared atmospheric sounding interferometer (IASI) (2011, background): “Since 1978, the Total Ozone Mapping Spectrometer (TOMS) (Krueger et al., 1995) and subsequent follow-up ozone monitoring instruments have been measuring SO2 through solar backscattered ultraviolet (BUV) measurements (see e.g.Yang et al., 2007, and references therein).”