Fig. 3
From: Arctic–Eurasian climate linkage induced by tropical ocean variability
Simulated surface climate anomalies in El Niño-decay year. Longitude–time section of sea surface temperature (SST) anomalies over 10°–20°N regressed onto ENSO(–1) in a HadISST (1958–2015) and b CESM1 ensemble mean (1958–2013). The time evolution is from January of ENSO-decaying year through June of the subsequent year. Regressed anomalies of c SST and d sea level pressure (SLP) in early winter onto ENSO(–1) for CESM1 ensemble mean. Black dotted contours and hatching in d indicate statistical significance at the p < 0.05 level
