Articles | Volume 20, issue 20
https://doi.org/10.5194/acp-20-11697-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-20-11697-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Impact of the eruption of Mt Pinatubo on the chemical composition of the stratosphere
Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
Sabine Brinkop
Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
Patrick Jöckel
Deutsches Zentrum für Luft- und Raumfahrt (DLR), Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany
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Cited
17 citations as recorded by crossref.
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- Estimating the impact of the 1991 Pinatubo eruption on mesospheric temperature by analyzing HALOE (UARS) temperature data S. Wallis et al. 10.5194/angeo-40-421-2022
- Spatio-temporal multivariate cluster evolution analysis for detecting and tracking climate impacts W. Iv et al. 10.1016/j.cam.2025.116583
- Comment on “Observation of large and all-season ozone losses over the tropics” [AIP Adv. 12, 075006 (2022)] M. Chipperfield et al. 10.1063/5.0121723
- Impact of a strong volcanic eruption on the summer middle atmosphere in UA-ICON simulations S. Wallis et al. 10.5194/acp-23-7001-2023
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- The Influence of Internal Climate Variability on Stratospheric Water Vapor Increases After Large‐Magnitude Explosive Tropical Volcanic Eruptions X. Zhou et al. 10.1029/2023GL103076
- Perturbation of Tropical Stratospheric Ozone Through Homogeneous and Heterogeneous Chemistry Due To Pinatubo Y. Peng et al. 10.1029/2023GL103773
- Rapid ozone depletion after humidification of the stratosphere by the Hunga Tonga Eruption S. Evan et al. 10.1126/science.adg2551
- The effect of ash, water vapor, and heterogeneous chemistry on the evolution of a Pinatubo-size volcanic cloud M. Abdelkader et al. 10.5194/acp-23-471-2023
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- The impact of volcanic eruptions of different magnitude on stratospheric water vapor in the tropics C. Kroll et al. 10.5194/acp-21-6565-2021
17 citations as recorded by crossref.
- What Contributes to the Inter‐Annual Variability in Tropical Lower Stratospheric Temperatures? A. Ming & P. Hitchcock 10.1029/2021JD035548
- Co-emission of volcanic sulfur and halogens amplifies volcanic effective radiative forcing J. Staunton-Sykes et al. 10.5194/acp-21-9009-2021
- Role of Stratospheric Processes in Climate Change: Advances and Challenges W. Tian et al. 10.1007/s00376-023-2341-1
- Estimating the impact of the 1991 Pinatubo eruption on mesospheric temperature by analyzing HALOE (UARS) temperature data S. Wallis et al. 10.5194/angeo-40-421-2022
- Spatio-temporal multivariate cluster evolution analysis for detecting and tracking climate impacts W. Iv et al. 10.1016/j.cam.2025.116583
- Comment on “Observation of large and all-season ozone losses over the tropics” [AIP Adv. 12, 075006 (2022)] M. Chipperfield et al. 10.1063/5.0121723
- Impact of a strong volcanic eruption on the summer middle atmosphere in UA-ICON simulations S. Wallis et al. 10.5194/acp-23-7001-2023
- Impact of Hunga Tonga-Hunga Ha’apai Volcanic Eruption on Stratospheric Water Vapour, Temperature, and Ozone G. Basha et al. 10.3390/rs15143602
- Atmospheric Chemistry Experiment (ACE) satellite observations of aerosols and SO2 emissions from the 2024 Ruang volcanic eruption R. Dodangodage et al. 10.1016/j.jqsrt.2024.109333
- The Influence of Internal Climate Variability on Stratospheric Water Vapor Increases After Large‐Magnitude Explosive Tropical Volcanic Eruptions X. Zhou et al. 10.1029/2023GL103076
- Perturbation of Tropical Stratospheric Ozone Through Homogeneous and Heterogeneous Chemistry Due To Pinatubo Y. Peng et al. 10.1029/2023GL103773
- Rapid ozone depletion after humidification of the stratosphere by the Hunga Tonga Eruption S. Evan et al. 10.1126/science.adg2551
- The effect of ash, water vapor, and heterogeneous chemistry on the evolution of a Pinatubo-size volcanic cloud M. Abdelkader et al. 10.5194/acp-23-471-2023
- Strong Evidence of Heterogeneous Processing on Stratospheric Sulfate Aerosol in the Extrapolar Southern Hemisphere Following the 2022 Hunga Tonga‐Hunga Ha'apai Eruption M. Santee et al. 10.1029/2023JD039169
- Random forest regression feature importance for climate impact pathway detection M. Brown et al. 10.1016/j.cam.2024.116479
- Investigating hydroclimatic impacts of the 168–158 BCE volcanic quartet and their relevance to the Nile River basin and Egyptian history R. Singh et al. 10.5194/cp-19-249-2023
- The impact of volcanic eruptions of different magnitude on stratospheric water vapor in the tropics C. Kroll et al. 10.5194/acp-21-6565-2021
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Short summary
After the volcanic eruption of Mt Pinatubo in 1991, ozone decreased in the tropics and increased in the midlatitudes and polar regions for 1 year. The change in the ozone column is solely a result of the volcanic heating, followed by an ozone decrease in the higher latitudes. This is caused by the volcanic aerosol, which changes the heterogeneous chemistry and thus the catalytic ozone loss cycles. Vertical transport of water vapour is enhanced by volcanic heating and increases methane.
After the volcanic eruption of Mt Pinatubo in 1991, ozone decreased in the tropics and increased...
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