Extended Data Fig. 3: Effect of NAO matching on trends during the decreasing-NAO period.
From: North Atlantic climate far more predictable than models imply
a–l, As in Extended Data Fig. 2, but over hindcast start dates of 1989–2005, inclusive. NAO matching improves the cooling trend over northern Eurasia, drying (wetting) over northern (southern) Europe and the increasing pressure trend across most of the Arctic.
