Anthropogenic Changes in Interannual-to-Decadal Climate Variability in CMIP6 Multiensemble Simulations

• Published in: Journal of Climate
• Main Authors: Coquereau, Arthur, Sévellec, Florian, Huck, Thierry, Hirschi, Joël J.-M., Hochet, Antoine
• Other Authors: Laboratoire d'Océanographie Physique et Spatiale (LOPS), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS), National Oceanography Centre Southampton (NOC), University of Southampton, CNRS/INSU/LEFE project ARVOR, ESA Living Planet Fellowship (PACIFIC project), ANR-17-EURE-0015,ISBlue,Interdisciplinary Graduate School for the Blue planet(2017), ANR-19-CHIA-0016,OceaniX,Physics-Informed AI for Observation-driven Ocean AnalytiX(2019)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2024
• Subjects: ENSO; Anthropogenic effects/forcing; Climate; Ensembles; Interannual variability; Internal variability; [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology; Sea ice
• Online Access: https://hal.science/hal-04685656; https://hal.science/hal-04685656/document; https://hal.science/hal-04685656/file/Coquereau_et_al_JC2024inpress.pdf; https://doi.org/10.1175/jcli-d-23-0606.1

International audience As well as having an impact on the background state of the climate, global warming due to human activities could affect its natural oscillations and internal variability. In this study, we use four initial-condition ensembles from the CMIP6 framework to investigate the potential evolution of internal climate variability under different warming pathways for the twenty-first century. Our results suggest significant changes in natural climate variability and point to two distinct regimes driving these changes. The first is a decrease in internal variability of surface air temperature at high latitudes and all frequencies, associated with a poleward shift and the gradual disappearance of sea ice edges, which we show to be an important component of internal variability. The second is an intensification of the interannual variability of surface air temperature and precipitation at low latitudes, which appears to be associated with El Niño–Southern Oscillation (ENSO). This second regime is particularly alarming because it may contribute to making the climate more unstable and less predictable, with a significant impact on human societies and ecosystems.