The Mediterranean climate change hotspot in the CMIP5 and CMIP6 projections
Abstract ∘ C in CMIP6 and 1.22 to 6.63 ∘ C in CMIP5 considering three different scenarios and the 50 % of inter-model spread by the end of the century. Contrarily to temperature projections, precipitation changes show greater uncertainties and spatial heterogeneity. However, a robust and significant precipitation decline is projected over large parts of the region during summer by the end of the century and for the high emission scenario (- - - - ∘ C before weighting to 0.68 ∘ C after weighting.
- Location
-
Deutsche Nationalbibliothek Frankfurt am Main
- Extent
-
Online-Ressource
- Language
-
Englisch
- Bibliographic citation
-
The Mediterranean climate change hotspot in the CMIP5 and CMIP6 projections ; volume:13 ; number:1 ; year:2022 ; pages:321-340 ; extent:20
Earth System Dynamics ; 13, Heft 1 (2022), 321-340 (gesamt 20)
- Creator
-
Cos, Josep
Doblas-Reyes, Francisco
Jury, Martin
Marcos, Raül
Bretonnière, Pierre-Antoine
Samsó, Margarida
- DOI
-
10.5194/esd-13-321-2022
- URN
-
urn:nbn:de:101:1-2022021004153221235923
- Rights
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
-
15.08.2025, 7:26 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Cos, Josep
- Doblas-Reyes, Francisco
- Jury, Martin
- Marcos, Raül
- Bretonnière, Pierre-Antoine
- Samsó, Margarida
Other Objects (12)
The Mediterranean climate change hotspot in the CMIP5 and CMIP6 projections
Uncertainty of ENSO-amplitude projections in CMIP5 and CMIP6 models
Uncertainty and hotspots in 21st century projections of agricultural drought from CMIP5 models
How well have CMIP3, CMIP5 and CMIP6 future climate projections portrayed the recently observed warming
How will southern hemisphere subtropical anticyclones respond to global warming? Mechanisms and seasonality in CMIP5 and CMIP6 model projections
Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6
Are Cut-off Lows simulated better in CMIP6 compared to CMIP5?
Using palaeo-climate comparisons to constrain future projections in CMIP5
Unterschiede zwischen den Ergebnissen der CMIP5 Modelle verwendet als Antrieb in EURO-CORDEX und dem gesamten CMIP5 und CMIP6 Ensemble
NASA Earth Exchange Downscaled Climate Projections 30 Arcseconds CMIP6
Emergent constraints on Equilibrium Climate Sensitivity in CMIP5: do they hold for CMIP6?
Emergent constraints on equilibrium climate sensitivity in CMIP5: do they hold for CMIP6?
The Mediterranean climate change hotspot in the CMIP5 and CMIP6 projections
Uncertainty of ENSO-amplitude projections in CMIP5 and CMIP6 models
Uncertainty and hotspots in 21st century projections of agricultural drought from CMIP5 models
How well have CMIP3, CMIP5 and CMIP6 future climate projections portrayed the recently observed warming
How will southern hemisphere subtropical anticyclones respond to global warming? Mechanisms and seasonality in CMIP5 and CMIP6 model projections
Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6
Are Cut-off Lows simulated better in CMIP6 compared to CMIP5?
Using palaeo-climate comparisons to constrain future projections in CMIP5
Unterschiede zwischen den Ergebnissen der CMIP5 Modelle verwendet als Antrieb in EURO-CORDEX und dem gesamten CMIP5 und CMIP6 Ensemble
NASA Earth Exchange Downscaled Climate Projections 30 Arcseconds CMIP6
Emergent constraints on Equilibrium Climate Sensitivity in CMIP5: do they hold for CMIP6?
Emergent constraints on equilibrium climate sensitivity in CMIP5: do they hold for CMIP6?
The Mediterranean climate change hotspot in the CMIP5 and CMIP6 projections
Uncertainty of ENSO-amplitude projections in CMIP5 and CMIP6 models
Uncertainty and hotspots in 21st century projections of agricultural drought from CMIP5 models
How well have CMIP3, CMIP5 and CMIP6 future climate projections portrayed the recently observed warming
How will southern hemisphere subtropical anticyclones respond to global warming? Mechanisms and seasonality in CMIP5 and CMIP6 model projections
Tracking Improvement in Simulated Marine Biogeochemistry Between CMIP5 and CMIP6
Are Cut-off Lows simulated better in CMIP6 compared to CMIP5?
Using palaeo-climate comparisons to constrain future projections in CMIP5
Unterschiede zwischen den Ergebnissen der CMIP5 Modelle verwendet als Antrieb in EURO-CORDEX und dem gesamten CMIP5 und CMIP6 Ensemble
NASA Earth Exchange Downscaled Climate Projections 30 Arcseconds CMIP6
Emergent constraints on Equilibrium Climate Sensitivity in CMIP5: do they hold for CMIP6?