Figure 2 | Scientific Reports

Figure 2

From: Modern and sub-fossil corals suggest reduced temperature variability in the eastern pole of the Indian Ocean Dipole during the medieval climate anomaly

Figure 2

Sea surface temperature variability at Enggano Island and Lampung Bay. (a–d) (left) Monthly SST (black lines), its anomaly (blue lines) and (right) its climatology. (e) Linear regression of monthly SST from Enggano Island versus SST from Lampung Bay. (f) Same as (e) but for monthly anomalies. SST data is from ERSSTv549 from the grid boxes including the coral sites, and displayed over the period of Nov 1968–Sep 2007: (a,b) Enggano Island (102.125 E 5.375 S) and (c,d) Lampung bay, Sunda strait (105.578 E 5.749 S).

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