Anticyclonic winds off Europe drive major shifts in Atlantic sea levels
Subtropical sea-surface height variability is influenced by winter North-Atlantic weather regimes. The Atlantic-Ridge (AR) weather regime has the strongest correlation with sea-level anomalies, impacting the subtropical gyre intensity. During AR events, anticyclonic wind anomalies off Europe shift wind-stress curl northward, affecting subtropical sea-surface height. This altered balance and ocean dynamics contribute to interannual variability in the Atlantic subtropical gyre. Winter season plays a key role in explaining the largest part of this variability, with AR being as important as the North Atlantic Oscillation (NAO).