Atmospheric centers of action: modern features and possible changes from simulations with CMIP6 and CMIP5 models

The results of an analysis of changes in the characteristics of atmospheric centers of action (ACAs) in the Northern (NH) and Southern (SH) hemispheres using results of simulations with the CMIP5 and CMIP6 ensembles of climate models are presented. The ability of models to simulate ACA features is estimated for the historical scenario in comparison with ERA5 reanalysis data. The projected changes are evaluated under RCP8.5 and SSP5-8.5 scenarios for CMIP5 and CMIP6 models, respectively. The ACA intensity is evaluated that defined as the difference in sea level pressure averaged over the ACA region and the entire hemisphere. In NH, reanalysis and models show greater intensity of subtropical oceanic anticyclonic ACAs in summer than in winter. The opposite is found for the intensity of NH subpolar oceanic cyclonic ACAs. The interannual variability of the ACA intensity in winter is generally greater than in summer. In SH, the season with greater intensity of oceanic anticyclonic and cyclonic ACAs and its interannual variability varies from ocean to ocean. CMIP5 and CMIP6 models show substantial changes of ACAs intensity in the ХХIst century. More significant trends in the strengthening of ACAs in the ХХIst century appear in the SH, especially in the winter seasons. The most consistent weakening trends are found over continents for winter North American maximum and the summer Asian minimum. For the winter Siberian maximum, the weakening trend is found more pronounced in CMIP6 models than in CMIP5.