Articles | Volume 14, issue 23
https://doi.org/10.5194/acp-14-13063-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-14-13063-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The impact of volcanic aerosol on the Northern Hemisphere stratospheric polar vortex: mechanisms and sensitivity to forcing structure
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
K. Krüger
GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
University of Oslo, Department of Geosciences, Oslo, Norway
M. Bittner
Max Planck Institute for Meteorology, Hamburg, Germany
International Max Planck Research School on Earth System Modeling (IMPRS), Hamburg, Germany
C. Timmreck
Max Planck Institute for Meteorology, Hamburg, Germany
H. Schmidt
Max Planck Institute for Meteorology, Hamburg, Germany
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Cited
32 citations as recorded by crossref.
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- Forecasting the climate response to volcanic eruptions: prediction skill related to stratospheric aerosol forcing M. Ménégoz et al. 10.1088/1748-9326/aac4db
- Significant Contributions of Volcanic Aerosols to Decadal Changes in the Stratospheric Circulation M. Diallo et al. 10.1002/2017GL074662
- Selective environmental stress from sulphur emitted by continental flood basalt eruptions A. Schmidt et al. 10.1038/ngeo2588
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- Modes of climate variability: Synthesis and review of proxy-based reconstructions through the Holocene A. Hernández et al. 10.1016/j.earscirev.2020.103286
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- The Circulation Response to Volcanic Eruptions: The Key Roles of Stratospheric Warming and Eddy Interactions K. DallaSanta et al. 10.1175/JCLI-D-18-0099.1
- 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
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- Unknown Eruption Source Parameters Cause Large Uncertainty in Historical Volcanic Radiative Forcing Reconstructions L. Marshall et al. 10.1029/2020JD033578
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- Radiative Forcing of Climate: The Historical Evolution of the Radiative Forcing Concept, the Forcing Agents and their Quantification, and Applications V. Ramaswamy et al. 10.1175/AMSMONOGRAPHS-D-19-0001.1
- Decadal Disruption of the QBO by Tropical Volcanic Supereruptions H. Brenna et al. 10.1029/2020GL089687
- Aerosol and Solar Irradiance Effects on Decadal Climate Variability and Predictability D. Zanchettin 10.1007/s40641-017-0065-y
- Stratospheric aerosol evolution after Pinatubo simulated with a coupled size-resolved aerosol–chemistry–climate model, SOCOL-AERv1.0 T. Sukhodolov et al. 10.5194/gmd-11-2633-2018
- The impact of wave-mean flow interaction on the Northern Hemisphere polar vortex after tropical volcanic eruptions M. Bittner et al. 10.1002/2015JD024603
- Is the Relationship Between Stratospheric Arctic Vortex and Arctic Oscillation Steady? D. Hu et al. 10.1029/2021JD035759
32 citations as recorded by crossref.
- Co-emission of volcanic sulfur and halogens amplifies volcanic effective radiative forcing J. Staunton-Sykes et al. 10.5194/acp-21-9009-2021
- Comparing the effects of solar-related and terrestrial drivers on the northern polar vortex A. Salminen et al. 10.1051/swsc/2020058
- Assessing the impact of a future volcanic eruption on decadal predictions S. Illing et al. 10.5194/esd-9-701-2018
- Northern Hemisphere continental winter warming following the 1991 Mt. Pinatubo eruption: reconciling models and observations L. Polvani et al. 10.5194/acp-19-6351-2019
- The Model Intercomparison Project on the climatic response to Volcanic forcing (VolMIP): experimental design and forcing input data for CMIP6 D. Zanchettin et al. 10.5194/gmd-9-2701-2016
- North Atlantic weather regimes in δ18O of winter precipitation: isotopic fingerprint of the response in the atmospheric circulation after volcanic eruptions H. GuðlaugsdÓttir et al. 10.1080/16000889.2019.1633848
- Scant evidence for a volcanically forced winter warming over Eurasia following the Krakatau eruption of August 1883 L. Polvani & S. Camargo 10.5194/acp-20-13687-2020
- Forecasting the climate response to volcanic eruptions: prediction skill related to stratospheric aerosol forcing M. Ménégoz et al. 10.1088/1748-9326/aac4db
- Significant Contributions of Volcanic Aerosols to Decadal Changes in the Stratospheric Circulation M. Diallo et al. 10.1002/2017GL074662
- Selective environmental stress from sulphur emitted by continental flood basalt eruptions A. Schmidt et al. 10.1038/ngeo2588
- The Interactive Stratospheric Aerosol Model Intercomparison Project (ISA-MIP): motivation and experimental design C. Timmreck et al. 10.5194/gmd-11-2581-2018
- Climate Impacts From Large Volcanic Eruptions in a High‐Resolution Climate Model: The Importance of Forcing Structure W. Yang et al. 10.1029/2019GL082367
- Modes of climate variability: Synthesis and review of proxy-based reconstructions through the Holocene A. Hernández et al. 10.1016/j.earscirev.2020.103286
- Reduced cooling following future volcanic eruptions P. Hopcroft et al. 10.1007/s00382-017-3964-7
- The Circulation Response to Volcanic Eruptions: The Key Roles of Stratospheric Warming and Eddy Interactions K. DallaSanta et al. 10.1175/JCLI-D-18-0099.1
- 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
- Modeling the 1783–1784 Laki Eruption in Iceland: 1. Aerosol Evolution and Global Stratospheric Circulation Impacts B. Zambri et al. 10.1029/2018JD029553
- 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
- A robust equatorial Pacific westerly response to tropical volcanism in multiple models J. Chai et al. 10.1007/s00382-020-05453-6
- The Arctic Polar Vortex Response to Volcanic Forcing of Different Strengths A. Azoulay et al. 10.1029/2020JD034450
- Using a large ensemble of simulations to assess the Northern Hemisphere stratospheric dynamical response to tropical volcanic eruptions and its uncertainty M. Bittner et al. 10.1002/2016GL070587
- Role of the Atlantic Multidecadal Variability in modulating the climate response to a Pinatubo-like volcanic eruption M. Ménégoz et al. 10.1007/s00382-017-3986-1
- The Influence of Stratospheric Soot and Sulfate Aerosols on the Northern Hemisphere Wintertime Atmospheric Circulation J. Coupe & A. Robock 10.1029/2020JD034513
- Unknown Eruption Source Parameters Cause Large Uncertainty in Historical Volcanic Radiative Forcing Reconstructions L. Marshall et al. 10.1029/2020JD033578
- Stratospheric aerosol-Observations, processes, and impact on climate S. Kremser et al. 10.1002/2015RG000511
- Changing transport processes in the stratosphere by radiative heating of sulfate aerosols U. Niemeier & H. Schmidt 10.5194/acp-17-14871-2017
- Radiative Forcing of Climate: The Historical Evolution of the Radiative Forcing Concept, the Forcing Agents and their Quantification, and Applications V. Ramaswamy et al. 10.1175/AMSMONOGRAPHS-D-19-0001.1
- Decadal Disruption of the QBO by Tropical Volcanic Supereruptions H. Brenna et al. 10.1029/2020GL089687
- Aerosol and Solar Irradiance Effects on Decadal Climate Variability and Predictability D. Zanchettin 10.1007/s40641-017-0065-y
- Stratospheric aerosol evolution after Pinatubo simulated with a coupled size-resolved aerosol–chemistry–climate model, SOCOL-AERv1.0 T. Sukhodolov et al. 10.5194/gmd-11-2633-2018
- The impact of wave-mean flow interaction on the Northern Hemisphere polar vortex after tropical volcanic eruptions M. Bittner et al. 10.1002/2015JD024603
- Is the Relationship Between Stratospheric Arctic Vortex and Arctic Oscillation Steady? D. Hu et al. 10.1029/2021JD035759
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Latest update: 30 May 2023
Short summary
Earth system model simulations are used to investigate the impact of volcanic aerosol forcing on stratospheric dynamics, e.g. the Northern Hemisphere (NH) polar vortex. We find that mechanisms linking aerosol heating and high-latitude dynamics are not as direct as often assumed; high-latitude effects result from changes in stratospheric circulation and related vertical motions. The simulated responses also show evidence of being sensitive to the structure of the volcanic forcing used.
Earth system model simulations are used to investigate the impact of volcanic aerosol forcing on...
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