Fig. 2
From: Robustness of the long-term nonlinear evolution of global sea surface temperature trend
The temporal locality of EEMD decomposition of the annual SSTA at a (42°S—46°S, 58°W—54°W) averaged in the South Atlantic; b (2°S—2°N, 122°W—118°W) averaged in the equatorial Pacific. From top to bottom, the curves represent the raw data, EEMD components (\({c}_{j}\)), and secular trend. The curves are colored from light to dark in each panel, representing 1900–2020, 1920–2020, and 1940–2020, respectively