A new study has revealed significant acceleration in the upper-ocean circulation of the equatorial Pacific over the past 30 years. This acceleration is primarily driven by intensified atmospheric winds, leading to increased oceanic currents that are both stronger and shallower, with potential impacts on regional and global climate patterns, including the frequency and intensity of El Niño and La Niña events. The study provides a spatial view of these long-term trends from observations, adding at least another decade of data from previous studies.
