SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE1530

Composite near-surface temperature anomalies (K) for the two following winters of the past nine most recent large tropical volcanic eruptions (Table 2) in all models and the

The interaction between the tropical SST and mid-high latitude atmospheric circulation has been a key topic in meteorology and oceanography since the pioneering works of

In contrast, the dominant sources of uncertainty for projections of decadally averaged relative SST and TS frequency are funda- mentally different (Fig. 3c,d), even though

(a) Time series of the area mean P anomaly difference (AMIP5 ensemble mean minus GPCP) over the tropical ocean, together with the five month running mean (thick black line) and

A coupled climate model is used to explore the response of the tropical sea surface temperature (SST) to positive SST anomalies in the global extratropics.. The main model results

Comparison of KM5c SST data relative to the pre-industrial period (NOAA-ERSST5) for global mean SST anomalies (SSTA) and the change in meridional SST gradient, constructed using

Interdecadal covariability of the ITCZ position and the North Atlantic high latitude climate seems to arise from low frequency atmospheric variability related to MOC variability..

4 shows that our coupled model reproduces the main tropical SST response to NIÑO34 (Fig. 4a), compared for instance with Cai et al. The patterns are displayed as amplitudes