Articles | Volume 7, issue 3
https://doi.org/10.5194/esd-7-681-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esd-7-681-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Hemispherically asymmetric volcanic forcing of tropical hydroclimate during the last millennium
Christopher M. Colose
CORRESPONDING AUTHOR
Dept. of Atmospheric & Environmental Sciences, University at Albany,
SUNY, Albany, NY 12222, USA
Allegra N. LeGrande
NASA Goddard Institute for Space Studies, New York, NY 10025, USA
Mathias Vuille
Dept. of Atmospheric & Environmental Sciences, University at Albany,
SUNY, Albany, NY 12222, USA
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64 citations as recorded by crossref.
- Role of eruption season in reconciling model and proxy responses to tropical volcanism S. Stevenson et al. 10.1073/pnas.1612505114
- Assessing response of local moisture conditions in central Brazil to variability in regional monsoon intensity using speleothem 87Sr/86Sr values B. Wortham et al. 10.1016/j.epsl.2017.01.034
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- Impact of volcanic aerosol hemispheric symmetry on Sahel rainfall T. Jacobson et al. 10.1007/s00382-020-05347-7
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- Fingerprint of volcanic forcing on the ENSO–Indian monsoon coupling M. Singh et al. 10.1126/sciadv.aba8164
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- Volcanic Eruption Signatures in the Isotope‐Enabled Last Millennium Ensemble S. Stevenson et al. 10.1029/2019PA003625
- Human influence on joint changes in temperature, rainfall and continental aridity C. Bonfils et al. 10.1038/s41558-020-0821-1
- Global hydroclimatic response to tropical volcanic eruptions over the last millennium E. Tejedor et al. 10.1073/pnas.2019145118
- Dwindling Relevance of Large Volcanic Eruptions for Global Glacier Changes in the Anthropocene M. Zemp & B. Marzeion 10.1029/2021GL092964
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- The sensitivity of the El Niño–Southern Oscillation to volcanic aerosol spatial distribution in the MPI Grand Ensemble B. Ward et al. 10.5194/esd-12-975-2021
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- Sensitivity of regional monsoons to idealised equatorial volcanic eruption of different sulfur emission strengths R. D’Agostino & C. Timmreck 10.1088/1748-9326/ac62af
- Investigating stable oxygen and carbon isotopic variability in speleothem records over the last millennium using multiple isotope-enabled climate models J. Bühler et al. 10.5194/cp-18-1625-2022
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- Hemispherically in-phase precipitation variability over the last 1700 years in a Madagascar speleothem record N. Scroxton et al. 10.1016/j.quascirev.2017.03.017
- European and Mediterranean hydroclimate responses to tropical volcanic forcing over the last millennium M. Rao et al. 10.1002/2017GL073057
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- Climate Variability, Volcanic Forcing, and Last Millennium Hydroclimate Extremes S. Stevenson et al. 10.1175/JCLI-D-17-0407.1
- Evaluating the link between the sulfur-rich Laacher See volcanic eruption and the Younger Dryas climate anomaly J. Baldini et al. 10.5194/cp-14-969-2018
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1 citations as recorded by crossref.
Discussed (final revised paper)
Latest update: 20 Nov 2024
Short summary
A band of intense rainfall exists near the equator known as the intertropical convergence zone, which can migrate in response to climate forcings. Here, we assess such migration in response to volcanic eruptions of varying spatial structure (Northern Hemisphere, Southern Hemisphere, or an eruption fairly symmetric about the equator). We do this using model simulations of the last millennium and link results to energetic constraints and the imprint eruptions may leave behind in past records.
A band of intense rainfall exists near the equator known as the intertropical convergence zone,...
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