Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-135-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-15-135-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The 4.2 ka event in the central Mediterranean: new data from a Corchia speleothem (Apuan Alps, central Italy)
Istituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy
Giovanni Zanchetta
Istituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy
Dipartimento di Scienze della Terra, University of Pisa, Pisa, Italy
Russell N. Drysdale
School of Geography, University of Melbourne, Melbourne, Australia
Eleonora Regattieri
Dipartimento di Scienze della Terra, University of Pisa, Pisa, Italy
School of Geography, University of Melbourne, Melbourne, Australia
Monica Bini
Istituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy
Dipartimento di Scienze della Terra, University of Pisa, Pisa, Italy
Petra Bajo
School of Earth Sciences, University of Melbourne, Melbourne, Australia
John C. Hellstrom
School of Earth Sciences, University of Melbourne, Melbourne, Australia
Ilaria Baneschi
Istituto di Geoscience e Georisorse-CNR, Pisa, Italy
Piero Lionello
Dipartimento Scienze e Tecnologie Biologiche e Ambientali, Università del Salento, Lecce, Italy
Jon Woodhead
School of Earth Sciences, University of Melbourne, Melbourne, Australia
Alan Greig
School of Earth Sciences, University of Melbourne, Melbourne, Australia
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34 citations as recorded by crossref.
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1 citations as recorded by crossref.
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
To understand the natural variability in the climate system, the hydrological aspect (dry and wet conditions) is particularly important for its impact on our societies. The reconstruction of past precipitation regimes can provide a useful tool for forecasting future climate changes. We use multi-proxy time series (oxygen and carbon isotopes, trace elements) from a speleothem to investigate circulation pattern variations and seasonality effects during the dry 4.2 ka event in central Italy.
To understand the natural variability in the climate system, the hydrological aspect (dry and...
Special issue