Articles | Volume 17, issue 6
Clim. Past, 17, 2607–2632, 2021
https://doi.org/10.5194/cp-17-2607-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue: Interdisciplinary studies of volcanic impacts on climate and...
Research article 20 Dec 2021
Research article | 20 Dec 2021
The blue suns of 1831: was the eruption of Ferdinandea, near Sicily, one of the largest volcanic climate forcing events of the nineteenth century?
Christopher Garrison et al.
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Marco Sacchi, Giuseppe De Natale, Volkhard Spiess, Lena Steinmann, Valerio Acocella, Marta Corradino, Shanaka de Silva, Alessandro Fedele, Lorenzo Fedele, Nobuo Geshi, Christopher Kilburn, Donatella Insinga, Maria-José Jurado, Flavia Molisso, Paola Petrosino, Salvatore Passaro, Fabrizio Pepe, Sabina Porfido, Claudio Scarpati, Hans-Ulrich Schmincke, Renato Somma, Mari Sumita, Stella Tamburrino, Claudia Troise, Mattia Vallefuoco, and Guido Ventura
Sci. Dril., 26, 29–46, https://doi.org/10.5194/sd-26-29-2019, https://doi.org/10.5194/sd-26-29-2019, 2019
Short summary
Short summary
A MagellanPlus workshop was held in Naples, Italy (25–28 February 2017), to explore the potential of the Campi Flegrei caldera as a target for an Amphibious Drilling Proposal to be submitted to international drilling programs. Campi Flegrei is an ideal natural laboratory to analyze the mechanisms of caldera dynamics and the relationships between hydrothermal and magmatic processes. The results will significantly advance our understanding of the most complex forms of volcanic structures on Earth.
Related subject area
Subject: Climate Modelling | Archive: Historical Records | Timescale: Holocene
Northern Hemisphere atmospheric pattern enhancing Eastern Mediterranean Transient-type events during the past 1000 years
Synergy of the westerly winds and monsoons in the lake evolution of global closed basins since the Last Glacial Maximum and implications for hydrological change in central Asia
A regional climate palaeosimulation for Europe in the period 1500–1990 – Part 2: Shortcomings and strengths of models and reconstructions
Simulated climate variability in the region of Rapa Nui during the last millennium
Aleix Cortina-Guerra, Juan José Gomez-Navarro, Belen Martrat, Juan Pedro Montávez, Alessandro Incarbona, Joan O. Grimalt, Marie-Alexandrine Sicre, and P. Graham Mortyn
Clim. Past, 17, 1523–1532, https://doi.org/10.5194/cp-17-1523-2021, https://doi.org/10.5194/cp-17-1523-2021, 2021
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During late 20th century a singular Mediterranean circulation episode called the Eastern Mediterranean Transient (EMT) event occurred. It involved changes on the seawater physical and biogeochemical properties, which can impact areas broadly. Here, using paleosimulations for the last 1000 years we found that the East Atlantic/Western Russian atmospheric mode was the main driver of the EMT-type events in the past, and enhancement of this mode was coetaneous with low solar insolation.
Yu Li and Yuxin Zhang
Clim. Past, 16, 2239–2254, https://doi.org/10.5194/cp-16-2239-2020, https://doi.org/10.5194/cp-16-2239-2020, 2020
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Monsoons and westerly winds interact with each other in the middle to low latitudes. We track millennial-scale evolution characteristics of monsoons and westerly winds over the past 21 000 years. In the monsoon-dominated regions of Asia, a humid climate prevails in the past 6000–10 000 years, while in the westerly-wind-dominated regions of Asia, the climate is relatively humid around 21 000 years and 6000 years ago.
J. J. Gómez-Navarro, O. Bothe, S. Wagner, E. Zorita, J. P. Werner, J. Luterbacher, C. C. Raible, and J. P Montávez
Clim. Past, 11, 1077–1095, https://doi.org/10.5194/cp-11-1077-2015, https://doi.org/10.5194/cp-11-1077-2015, 2015
C. Junk and M. Claussen
Clim. Past, 7, 579–586, https://doi.org/10.5194/cp-7-579-2011, https://doi.org/10.5194/cp-7-579-2011, 2011
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Short summary
An unidentified eruption in 1831 was one of the largest volcanic climate forcing events of the nineteenth century. We use reported observations of a blue sun to reconstruct the transport of an aerosol plume from that eruption and, hence, identify it as the 1831 eruption of Ferdinandea, near Sicily. We propose that, although it was only a modest eruption, its volcanic plume was enriched with sulfur from sedimentary deposits and that meteorological conditions helped it reach the stratosphere.
An unidentified eruption in 1831 was one of the largest volcanic climate forcing events of the...