Fig. 5
From: Enhanced climate instability in the North Atlantic and southern Europe during the Last Interglacial
Results of a suite of LOVECLIM experiments performed under LIG conditions. Control experiment is shown in black and experiments where 0.05 Sv (FWF005) and 0.03 Sv (FWF003) of freshwater was added to the area south of Greenland for 400 years are shown in blue and cyan, respectively (see Methods). Time series of: a meltwater input in the North Atlantic; b maximum overturning circulation in the North Atlantic; c North Atlantic current strength (44°W–36°W, 45°N–47°N, 0–54 m); d East Greenland current (45°W–32°W, 56°N–68°N, 0–694 m); e SST anomalies averaged around Iceland (26°W–18°W, 60°N–64°N); f SST anomalies averaged around the Labrador Sea (60°W–40°W, 56°N– 60°N); g SST anomalies averaged around the North Atlantic (40°W–30°W, 50°N–58°N); h annual mean precipitation anomaly averaged over Southern Europe (10°W–20°E, 36°N–46°N); i δ13C anomalies averaged over 47°W–40°W, 47°N–51°N, 3300–4020 m (blue and cyan circles) and over 24°W–18°W, 56°N–62°N, 1443–1992 m (magenta triangles). To highlight the centennial-scale variability, time series b through h have been smoothed by a 21-year running mean
