Articles | Volume 20, issue 11
https://doi.org/10.5194/acp-20-6521-2020
© 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-20-6521-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
05 Jun 2020
Research article |
| 05 Jun 2020
| 05 Jun 2020
The potential impacts of a sulfur- and halogen-rich supereruption such as Los Chocoyos on the atmosphere and climate
Hans Brenna
Section for Meteorology and Oceanography (MetOs), Department of Geosciences,
University of Oslo, P.O. Box 1022, Blindern, 0315, Oslo, Norway
now at: The Norwegian Meteorological Institute,
Oslo, Norway
Invited contribution by Hans Brenna, recipient of the European Geosciences Union (EGU) Atmospheric Sciences 2018 Outstanding Student Poster and PICO (OSPP) Award.
Steffen Kutterolf
GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstrasse 1–3, 24148 Kiel, Germany
Michael J. Mills
Atmospheric Chemistry Observations & Modeling, National Center for Atmospheric Research, P.O. Box 3000, Boulder, Colorado
80307-3000, USA
Section for Meteorology and Oceanography (MetOs), Department of Geosciences,
University of Oslo, P.O. Box 1022, Blindern, 0315, Oslo, Norway
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Cited
22 citations as recorded by crossref.
- Reconciling the climate and ozone response to the 1257 CE Mount Samalas eruption D. Wade et al. 10.1073/pnas.1919807117
- The 852/3 CE Mount Churchill eruption: examining the potential climatic and societal impacts and the timing of the Medieval Climate Anomaly in the North Atlantic region H. Mackay et al. 10.5194/cp-18-1475-2022
- The significance of volcanic ash in Greenland ice cores during the Common Era G. Plunkett et al. 10.1016/j.quascirev.2022.107936
- Climate change modulates the stratospheric volcanic sulfate aerosol lifecycle and radiative forcing from tropical eruptions T. Aubry et al. 10.1038/s41467-021-24943-7
- Bipolar ice-core records constrain possible dates and global radiative forcing following the ∼74 ka Toba eruption J. Lin et al. 10.1016/j.quascirev.2023.108162
- On Synchronous Supereruptions A. Cisneros de León et al. 10.3389/feart.2022.827252
- Millimetre‐scale pollen analysis of non‐varved lacustrine sediments from Onepoto maar palaeolake, Auckland, reveals distal vegetation responses and landscape recovery following the ~25.5‐ka Ōruanui supereruption, New Zealand S. Piva et al. 10.1002/jqs.3506
- Rapid Determination of Sulfur in Sixty Geological Reference Materials by High Resolution Inductively Coupled Plasma‐Mass Spectrometry X. Qiu et al. 10.1111/ggr.12453
- Initial atmospheric conditions control transport of volcanic volatiles, forcing and impacts Z. Zhuo et al. 10.5194/acp-24-6233-2024
- Temporal characteristics of a 6.2 Ma-long ash-fall history in the NW Pacific E. Zelenin et al. 10.1016/j.jvolgeores.2024.108141
- A history of violence: magma incubation, timing and tephra distribution of the Los Chocoyos supereruption (Atitlán Caldera, Guatemala) A. Cisneros de León et al. 10.1002/jqs.3265
- Observation and modelling of ozone-destructive halogen chemistry in a passively degassing volcanic plume L. Surl et al. 10.5194/acp-21-12413-2021
- The Toba supervolcano eruption caused severe tropical stratospheric ozone depletion S. Osipov et al. 10.1038/s43247-021-00141-7
- Volcanic forcing of high-latitude Northern Hemisphere eruptions H. Fuglestvedt et al. 10.1038/s41612-023-00539-4
- The impact of volcanic emission of halogenated compounds on the Southern Hemisphere and Antarctic environment M. Basylevska & V. Bogillo 10.33275/1727-7485.2.2021.675
- 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
- Co-emission of volcanic sulfur and halogens amplifies volcanic effective radiative forcing J. Staunton-Sykes et al. 10.5194/acp-21-9009-2021
- Zircon and Melt Extraction From a Long‐Lived and Vertically Extensive Magma System Underneath Ilopango Caldera (El Salvador) A. Cisneros de León et al. 10.1029/2020GC009507
- Sensitivity of stratospheric ozone to the latitude, season, and halogen content of a contemporary explosive volcanic eruption F. Østerstrøm et al. 10.1038/s41598-023-32574-9
- Decadal Disruption of the QBO by Tropical Volcanic Supereruptions H. Brenna et al. 10.1029/2020GL089687
- Dwindling Relevance of Large Volcanic Eruptions for Global Glacier Changes in the Anthropocene M. Zemp & B. Marzeion 10.1029/2021GL092964
- A Bayesian age from dispersed plagioclase and zircon dates in the Los Chocoyos ash, Central America A. Baudry et al. 10.1016/j.epsl.2024.118826
22 citations as recorded by crossref.
- Reconciling the climate and ozone response to the 1257 CE Mount Samalas eruption D. Wade et al. 10.1073/pnas.1919807117
- The 852/3 CE Mount Churchill eruption: examining the potential climatic and societal impacts and the timing of the Medieval Climate Anomaly in the North Atlantic region H. Mackay et al. 10.5194/cp-18-1475-2022
- The significance of volcanic ash in Greenland ice cores during the Common Era G. Plunkett et al. 10.1016/j.quascirev.2022.107936
- Climate change modulates the stratospheric volcanic sulfate aerosol lifecycle and radiative forcing from tropical eruptions T. Aubry et al. 10.1038/s41467-021-24943-7
- Bipolar ice-core records constrain possible dates and global radiative forcing following the ∼74 ka Toba eruption J. Lin et al. 10.1016/j.quascirev.2023.108162
- On Synchronous Supereruptions A. Cisneros de León et al. 10.3389/feart.2022.827252
- Millimetre‐scale pollen analysis of non‐varved lacustrine sediments from Onepoto maar palaeolake, Auckland, reveals distal vegetation responses and landscape recovery following the ~25.5‐ka Ōruanui supereruption, New Zealand S. Piva et al. 10.1002/jqs.3506
- Rapid Determination of Sulfur in Sixty Geological Reference Materials by High Resolution Inductively Coupled Plasma‐Mass Spectrometry X. Qiu et al. 10.1111/ggr.12453
- Initial atmospheric conditions control transport of volcanic volatiles, forcing and impacts Z. Zhuo et al. 10.5194/acp-24-6233-2024
- Temporal characteristics of a 6.2 Ma-long ash-fall history in the NW Pacific E. Zelenin et al. 10.1016/j.jvolgeores.2024.108141
- A history of violence: magma incubation, timing and tephra distribution of the Los Chocoyos supereruption (Atitlán Caldera, Guatemala) A. Cisneros de León et al. 10.1002/jqs.3265
- Observation and modelling of ozone-destructive halogen chemistry in a passively degassing volcanic plume L. Surl et al. 10.5194/acp-21-12413-2021
- The Toba supervolcano eruption caused severe tropical stratospheric ozone depletion S. Osipov et al. 10.1038/s43247-021-00141-7
- Volcanic forcing of high-latitude Northern Hemisphere eruptions H. Fuglestvedt et al. 10.1038/s41612-023-00539-4
- The impact of volcanic emission of halogenated compounds on the Southern Hemisphere and Antarctic environment M. Basylevska & V. Bogillo 10.33275/1727-7485.2.2021.675
- 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
- Co-emission of volcanic sulfur and halogens amplifies volcanic effective radiative forcing J. Staunton-Sykes et al. 10.5194/acp-21-9009-2021
- Zircon and Melt Extraction From a Long‐Lived and Vertically Extensive Magma System Underneath Ilopango Caldera (El Salvador) A. Cisneros de León et al. 10.1029/2020GC009507
- Sensitivity of stratospheric ozone to the latitude, season, and halogen content of a contemporary explosive volcanic eruption F. Østerstrøm et al. 10.1038/s41598-023-32574-9
- Decadal Disruption of the QBO by Tropical Volcanic Supereruptions H. Brenna et al. 10.1029/2020GL089687
- Dwindling Relevance of Large Volcanic Eruptions for Global Glacier Changes in the Anthropocene M. Zemp & B. Marzeion 10.1029/2021GL092964
- A Bayesian age from dispersed plagioclase and zircon dates in the Los Chocoyos ash, Central America A. Baudry et al. 10.1016/j.epsl.2024.118826
Latest update: 10 Oct 2024
Short summary
The Los Chocoyos supereruption (84 000 years ago) in Guatemala was one of the largest volcanic events of the last 100 000 years. This eruption released enormous amounts of sulfur, which cooled the climate, as well as chlorine and bromine, which destroyed the ozone in the stratosphere. We have simulated this eruption by using an advanced chemistry–climate model. We found a collapse in the ozone layer lasting more than 10 years, increased surface–UV radiation, and a 30-year climate-cooling period.
The Los Chocoyos supereruption (84 000 years ago) in Guatemala was one of the largest volcanic...
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