Author

B. Castelle

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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