Articles | Volume 17, issue 7
Atmos. Chem. Phys., 17, 4857–4870, 2017
https://doi.org/10.5194/acp-17-4857-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 17, 4857–4870, 2017
https://doi.org/10.5194/acp-17-4857-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
13 Apr 2017
Research article
| 13 Apr 2017
Space-based observation of volcanic iodine monoxide
Anja Schönhardt et al.
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Cited
12 citations as recorded by crossref.
- Global ozone depletion and increase of UV radiation caused by pre-industrial tropical volcanic eruptions H. Brenna et al. 10.1038/s41598-019-45630-0
- The potential impacts of a sulfur- and halogen-rich supereruption such as Los Chocoyos on the atmosphere and climate H. Brenna et al. 10.5194/acp-20-6521-2020
- Ozone Depletion in Tropospheric Volcanic Plumes: From Halogen-Poor to Halogen-Rich Emissions T. Roberts 10.3390/geosciences8020068
- Halogen activation in the plume of Masaya volcano: field observations and box model investigations J. Rüdiger et al. 10.5194/acp-21-3371-2021
- Kinetics of the Reactions of Ozone with Halogen Atoms in the Stratosphere S. Vijayakumar et al. 10.3390/atmos12081053
- Ozone depletion due to dust release of iodine in the free troposphere T. Koenig et al. 10.1126/sciadv.abj6544
- First high-resolution BrO column retrievals from TROPOMI S. Seo et al. 10.5194/amt-12-2913-2019
- High-Resolution Photoelectron Imaging and Photodetachment Spectroscopy of Cryogenically Cooled IO– Y. Wang et al. 10.1021/acs.jpca.0c04080
- Iodine chemistry in the chemistry–climate model SOCOL-AERv2-I A. Karagodin-Doyennel et al. 10.5194/gmd-14-6623-2021
- Development and application of a sampling method for the determination of reactive halogen species in volcanic gas emissions J. Rüdiger et al. 10.1007/s00216-017-0525-1
- Advances in Bromine Speciation in Volcanic Plumes A. Gutmann et al. 10.3389/feart.2018.00213
- Periodicity in Volcanic Gas Plumes: A Review and Analysis . Pering et al. 10.3390/geosciences9090394
12 citations as recorded by crossref.
- Global ozone depletion and increase of UV radiation caused by pre-industrial tropical volcanic eruptions H. Brenna et al. 10.1038/s41598-019-45630-0
- The potential impacts of a sulfur- and halogen-rich supereruption such as Los Chocoyos on the atmosphere and climate H. Brenna et al. 10.5194/acp-20-6521-2020
- Ozone Depletion in Tropospheric Volcanic Plumes: From Halogen-Poor to Halogen-Rich Emissions T. Roberts 10.3390/geosciences8020068
- Halogen activation in the plume of Masaya volcano: field observations and box model investigations J. Rüdiger et al. 10.5194/acp-21-3371-2021
- Kinetics of the Reactions of Ozone with Halogen Atoms in the Stratosphere S. Vijayakumar et al. 10.3390/atmos12081053
- Ozone depletion due to dust release of iodine in the free troposphere T. Koenig et al. 10.1126/sciadv.abj6544
- First high-resolution BrO column retrievals from TROPOMI S. Seo et al. 10.5194/amt-12-2913-2019
- High-Resolution Photoelectron Imaging and Photodetachment Spectroscopy of Cryogenically Cooled IO– Y. Wang et al. 10.1021/acs.jpca.0c04080
- Iodine chemistry in the chemistry–climate model SOCOL-AERv2-I A. Karagodin-Doyennel et al. 10.5194/gmd-14-6623-2021
- Development and application of a sampling method for the determination of reactive halogen species in volcanic gas emissions J. Rüdiger et al. 10.1007/s00216-017-0525-1
- Advances in Bromine Speciation in Volcanic Plumes A. Gutmann et al. 10.3389/feart.2018.00213
- Periodicity in Volcanic Gas Plumes: A Review and Analysis . Pering et al. 10.3390/geosciences9090394
Latest update: 08 Aug 2022
Short summary
Iodine monoxide, IO, is observed in satellite measurements following the eruption of the Kasatochi volcano, Alaska, in August 2008. Large IO columns are detected by SCIAMACHY on ENVISAT and by GOME-2 on MetOp-A for several days. IO amounts are approximately 1 order of magnitude smaller than those of BrO. Details in the spatial distributions differ between IO, BrO and sulfur dioxide, SO2. The total mass of IO in the volcanic plume is determined to be on the order of 10 Mg.
Iodine monoxide, IO, is observed in satellite measurements following the eruption of the...
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