Future evolution of Marine Heatwaves in the Mediterranean Sea
Autor: | Dmitry Sein, William Cabos Narváez, Samuel Somot, Pierre Nabat, Gianmaria Sannino, Florence Sevault, Sofia Darmaraki, Vladimir Djurdjevic, Laurent Li, Leone Cavicchia |
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Přispěvatelé: | Darmaraki, S., Somot, S., Sevault, F., Nabat, P., Cabos Narvaez, W. D., Cavicchia, L., Djurdjevic, V., Li, L., Sannino, G., Sein, D. V., Groupe de Météorologie de Grande Échelle et Climat (GMGEC), Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL) |
Jazyk: | angličtina |
Rok vydání: | 2019 |
Předmět: |
Atmospheric Science
Extreme ocean temperature Marine Heatwaves 010504 meteorology & atmospheric sciences Future scenario Effects of global warming on oceans Coupled regional climate models Climate change Forcing (mathematics) Structural basin 010502 geochemistry & geophysics 01 natural sciences Med-CORDEX Mediterranean sea Coupled regional climate model Mediterranean Sea Marine ecosystem 14. Life underwater Marine Heatwave 0105 earth and related environmental sciences Climate simulation Climate simulations Extreme ocean temperatures 13. Climate action [SDU]Sciences of the Universe [physics] Climatology Greenhouse gas Period (geology) Environmental science |
Zdroj: | EPIC3Climate Dynamics, SPRINGER, ISSN: 0930-7575 Climate Dynamics Climate Dynamics, 2019, 53, pp.1371-1392. ⟨10.1007/s00382-019-04661-z⟩ |
ISSN: | 0930-7575 1432-0894 |
DOI: | 10.1007/s00382-019-04661-z⟩ |
Popis: | International audience; Extreme ocean warming events, known as marine heatwaves (MHWs), have been observed to perturb significantly marine ecosystems and fisheries around the world. Here, we propose a detection method for long-lasting and large-scale summer MHWs, using a local, climatological 99th percentile threshold, based on present-climate (1976-2005) daily SST. To assess their future evolution in the Mediterranean Sea we use, for the first time, a dedicated ensemble of fully-coupled Regional Climate System Models from the Med-CORDEX initiative and a multi-scenario approach. The models appear to simulate well MHW properties during historical period, despite biases in mean and extreme SST. In response to increasing greenhouse gas forcing, the events become stronger and more intense under RCP4.5 and RCP8.5 than RCP2.6. By 2100 and under RCP8.5, simulations project at least one long-lasting MHW every year, up to three months longer, about 4 times more intense and 42 times more severe than present-day events. They are expected to occur from June-October and to affect at peak the entire basin. Their evolution is found to occur mainly due to an increase in the mean SST, but increased daily SST variability also plays a noticeable role. Until the mid-21st century, MHW characteristics rise independently of the choice of the emission scenario, the influence of which becomes more evident by the end of the period. Further analysis reveals different climate change responses in certain configurations, more likely linked to their driving global climate model rather than to the individual model biases. |
Databáze: | OpenAIRE |
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