2005
DOI: 10.1007/s10874-005-5544-1
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On the Retrieval of Volcanic Sulfur Dioxide Emissions from GOME Backscatter Measurements

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Cited by 71 publications
(57 citation statements)
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“…Over the last decades, a host of satellite-based UV-visible instruments have been used for the monitoring of anthropogenic and volcanic SO 2 emissions. Total vertical column density (VCD) of SO 2 has been retrieved with the sensors TOMS (Krueger, 1983), GOME (Eisinger and Burrows, 1998;Thomas et al, 2005;Khokar et al, 2005), SCIAMACHY (Afe et al, 2004), OMI (Krotkov et al, 2006;Yang et al, 2007Yang et al, , 2010Li et al, 2013;Theys et al, 2015), GOME-2 Bobrowski et al, 2010;Nowlan et al, 2011;Rix et al, 2012;Hörmann et al, 2013) and OMPS . In particular, the Ozone Monitoring Instrument (OMI) has largely demonstrated the value of satellite UV-visible remote sensing (1) in monitoring volcanic plumes in near-real time (Brenot et al, 2014) and changes in volcanic degassing at the global scale , and references therein) and (2) in detecting and quantifying large anthropogenic SO 2 emissions, weak or N. Theys et al: S-5P SO 2 algorithm theoretical basis unreported emission sources worldwide (Theys et al, 2015;Fioletov et al, 2016;McLinden et al, 2016) as well as investigating their long-term changes van der A et al, 2016;He et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…Over the last decades, a host of satellite-based UV-visible instruments have been used for the monitoring of anthropogenic and volcanic SO 2 emissions. Total vertical column density (VCD) of SO 2 has been retrieved with the sensors TOMS (Krueger, 1983), GOME (Eisinger and Burrows, 1998;Thomas et al, 2005;Khokar et al, 2005), SCIAMACHY (Afe et al, 2004), OMI (Krotkov et al, 2006;Yang et al, 2007Yang et al, , 2010Li et al, 2013;Theys et al, 2015), GOME-2 Bobrowski et al, 2010;Nowlan et al, 2011;Rix et al, 2012;Hörmann et al, 2013) and OMPS . In particular, the Ozone Monitoring Instrument (OMI) has largely demonstrated the value of satellite UV-visible remote sensing (1) in monitoring volcanic plumes in near-real time (Brenot et al, 2014) and changes in volcanic degassing at the global scale , and references therein) and (2) in detecting and quantifying large anthropogenic SO 2 emissions, weak or N. Theys et al: S-5P SO 2 algorithm theoretical basis unreported emission sources worldwide (Theys et al, 2015;Fioletov et al, 2016;McLinden et al, 2016) as well as investigating their long-term changes van der A et al, 2016;He et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…This effect is corrected by applying background correction method used by various studies (e.g., Khokhar et al, 2005;Lee et al, 2009) An air mass factor (AMF) is mandatory for the conversion of the retrieved slant column-integrated along the light path, into a vertical column densities (VCD-generally expressed in Dobson unit -1 DU = 2.69 × 10 16 molecules/cm 2 ). The SO 2 AMF depends strongly on surface albedo, clouds, aerosols optical properties, the vertical distribution of SO 2 , and the ozone column (Khokhar et al, 2005;Thomas et al, 2005;Khokhar et al, 2008;Krotkov et al, 2008;Lee et al, 2009).…”
Section: So 2 Retrieval Analysismentioning
confidence: 99%
“…In order to attribute increased SO 2 values as found in satellite-based observations to a particular volcano or an active volcanic region, we apply the trajectory matching technique (Thomas et al, 2005). By means of calculating ensembles of backward trajectories starting from enhanced SO 2 column observations, the volcanic origin of such SO 2 plumes can be identified or rejected.…”
Section: Trajectory Analysismentioning
confidence: 99%
“…By matching the parcel trajectories with the first guess satellite-based SO 2 retrievals the height of the SO 2 plume is determined. The accuracy of the combined retrieval and trajectory matching approach was evaluated in Thomas et al (2005) using ground-based measurements of SO 2 and aerosols.…”
Section: Trajectory Analysismentioning
confidence: 99%