Anthropogenic Disruption of Orbital‐Scale Seasonal Asynchrony in the Tropical Pacific Walker Circulation During the Holocene
The zonal sea surface temperature gradient (SSTG) in the tropical Pacific governs the Pacific Walker Circulation (PWC) and global hydroclimate. Although the annual‐mean PWC is thought to have declined since the Mid‐Holocene, the seasonal architecture of its response to external forcing remains poorly constrained, obscu...