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International Journal of Climatology · 2009 · Vol. 29 · Issue 1 · Wiley
Air temperature anomalies over eastern North America and Europe are analysed during the extreme phases of the two leading low‐frequency modes of North Atlantic sea surface temperature (SST) during the 1906–2005 period. The leading mode of SST is a multi‐decadal signal—commonly referred to as the Atlantic multi‐decadal oscillation—with uniform polarity over the North Atlantic. Air temperature anomalies over the eastern United S...