Articles | Volume 18, issue 3
https://doi.org/10.5194/os-18-839-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-18-839-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
08 Jun 2022
Research article |
| 08 Jun 2022
| 08 Jun 2022
Seasonal extrema of sea surface temperature in CMIP6 models
Yanxin Wang
Centre for Ocean and Atmospheric Sciences, University of East Anglia, Norwich, UK
Centre for Ocean and Atmospheric Sciences, University of East Anglia, Norwich, UK
David P. Stevens
Centre for Ocean and Atmospheric Sciences, University of East Anglia, Norwich, UK
Gillian M. Damerell
Centre for Ocean and Atmospheric Sciences, University of East Anglia, Norwich, UK
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Cited
14 citations as recorded by crossref.
- Coastal warming under climate change: Global, faster and heterogeneous R. Varela et al. 10.1016/j.scitotenv.2023.164029
- The Role of Mesoscale Cloud Morphology in the Shortwave Cloud Feedback I. McCoy et al. 10.1029/2022GL101042
- Two‐way feedback between the Madden–Julian Oscillation and diurnal warm layers in a coupled ocean–atmosphere model E. Karlowska et al. 10.1002/qj.4807
- Atmospheric bias teleconnections in boreal winter associated with systematic sea surface temperature errors in the tropical Indian Ocean Y. Zhao et al. 10.5194/wcd-4-833-2023
- Air–sea heat fluxes variations in the Southern Atlantic Ocean: Present‐day and future climate scenarios R. Moura et al. 10.1002/joc.8517
- Divergent future change in South Atlantic Ocean Dipole impacts on regional rainfall in CMIP6 models U. Nworgu et al. 10.1088/2752-5295/ad3a0e
- Highly stratified mid-Pliocene Southern Ocean in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-20-1067-2024
- Examining the Ability of CMIP6 Models to Reproduce the Upwelling SST Imprint in the Eastern Boundary Upwelling Systems R. Varela et al. 10.3390/jmse10121970
- The effect of diurnal warming of sea‐surface temperatures on the propagation speed of the Madden–Julian oscillation E. Karlowska et al. 10.1002/qj.4599
- Assessment of hydrographic features in OMIP2 models in the Tropical Indian Ocean B. Madhu et al. 10.1007/s10236-025-01664-9
- Evaluation of multi-season convection-permitting atmosphere – mixed-layer ocean simulations of the Maritime Continent E. Howard et al. 10.5194/gmd-17-3815-2024
- On warm bias and mesoscale dynamics setting the Southern Ocean large-scale circulation mean state M. Zeller & T. Martin 10.1016/j.ocemod.2024.102426
- Characterisation of the observed diurnal cycle of precipitation over the Maritime Continent J. Mustafa et al. 10.1002/qj.4725
- Dynamics of the Atlantic Marine Intertropical Convergence Zone H. Giordani & P. Peyrillé 10.1029/2021JD036392
13 citations as recorded by crossref.
- Coastal warming under climate change: Global, faster and heterogeneous R. Varela et al. 10.1016/j.scitotenv.2023.164029
- The Role of Mesoscale Cloud Morphology in the Shortwave Cloud Feedback I. McCoy et al. 10.1029/2022GL101042
- Two‐way feedback between the Madden–Julian Oscillation and diurnal warm layers in a coupled ocean–atmosphere model E. Karlowska et al. 10.1002/qj.4807
- Atmospheric bias teleconnections in boreal winter associated with systematic sea surface temperature errors in the tropical Indian Ocean Y. Zhao et al. 10.5194/wcd-4-833-2023
- Air–sea heat fluxes variations in the Southern Atlantic Ocean: Present‐day and future climate scenarios R. Moura et al. 10.1002/joc.8517
- Divergent future change in South Atlantic Ocean Dipole impacts on regional rainfall in CMIP6 models U. Nworgu et al. 10.1088/2752-5295/ad3a0e
- Highly stratified mid-Pliocene Southern Ocean in PlioMIP2 J. Weiffenbach et al. 10.5194/cp-20-1067-2024
- Examining the Ability of CMIP6 Models to Reproduce the Upwelling SST Imprint in the Eastern Boundary Upwelling Systems R. Varela et al. 10.3390/jmse10121970
- The effect of diurnal warming of sea‐surface temperatures on the propagation speed of the Madden–Julian oscillation E. Karlowska et al. 10.1002/qj.4599
- Assessment of hydrographic features in OMIP2 models in the Tropical Indian Ocean B. Madhu et al. 10.1007/s10236-025-01664-9
- Evaluation of multi-season convection-permitting atmosphere – mixed-layer ocean simulations of the Maritime Continent E. Howard et al. 10.5194/gmd-17-3815-2024
- On warm bias and mesoscale dynamics setting the Southern Ocean large-scale circulation mean state M. Zeller & T. Martin 10.1016/j.ocemod.2024.102426
- Characterisation of the observed diurnal cycle of precipitation over the Maritime Continent J. Mustafa et al. 10.1002/qj.4725
1 citations as recorded by crossref.
Latest update: 08 Aug 2025
Short summary
It is important that climate models give accurate projections of future extremes in summer and winter sea surface temperature because these affect many features of the global climate system. Our results demonstrate that some models would give large errors if used for future projections of these features, and models with more detailed representation of vertical structure in the ocean tend to have a better representation of sea surface temperature, particularly in summer.
It is important that climate models give accurate projections of future extremes in summer and...
