Open access
Oct 2026
A persistent atmospheric pressure mode governs western Europe’s seasonal climate
The North Atlantic Oscillation (NAO) is widely recognised as the leading mode of atmospheric variability over the North Atlantic (90° W–40° E, 20°–80° N). However, its broad-scale dipole fails to fully explain climate variability at mid-latitudes around Western Europe, where coastal storm and hydroclimatic impacts rema...
R. Alkama, D. Swingedouw, B. Castelle et al.
· Climate Dynamics · 1 citation