Articles | Volume 11, issue 3
https://doi.org/10.5194/esd-11-793-2020
© 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/esd-11-793-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Compound warm–dry and cold–wet events over the Mediterranean
Department of Water and Climate Risk, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
Department of Earth Sciences, Uppsala University and Centre of Natural Hazards and Disaster Science (CNDS), Uppsala, Sweden
Gabriele Messori
Department of Earth Sciences, Uppsala University and Centre of Natural Hazards and Disaster Science (CNDS), Uppsala, Sweden
Department of Meteorology, Stockholm University and Bolin Centre for Climate Research, Stockholm, Sweden
Davide Faranda
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, CEA-CNRS-UVSQ, Université Paris-Saclay, Gif-sur-Yvette, France
London Mathematical Laboratory, London, UK
Philip J. Ward
Department of Water and Climate Risk, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
Dim Coumou
Department of Water and Climate Risk, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
Royal Netherlands Meteorological Institute (KNMI), De Bilt, the Netherlands
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Discussed (final revised paper)
Latest update: 22 Nov 2024
Short summary
In this paper we quantify Mediterranean compound temperature and precipitation dynamical extremes (CDEs) over the 1979–2018 period. The strength of the temperature–precipitation coupling during summer increased and is driven by surface warming. We also link the CDEs to compound hot–dry and cold–wet events during summer and winter respectively.
In this paper we quantify Mediterranean compound temperature and precipitation dynamical...
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