Why Atlantic and Pacific Sea Levels Differ
It's Not a Single Level
Mean sea level differs between ocean basins due to:
- Basin Geometry – Atlantic's narrow, meridional shape vs. Pacific's broad, zonal expanse alters circulation and steric height.
- Earth's Rotation (Coriolis) – Deflects flows, creating western boundary currents (Gulf Stream, Kuroshio) that pile water against western margins.
- Temperature/Salinity (Density) – Atlantic is saltier and cooler → denser water → lower steric height *locally*, but large-scale circulation redistributes mass.
- Land Barriers – Americas block direct Pacific-Atlantic exchange (except Drake Passage, Indonesian Throughflow).
- Climate Change – Non-uniform thermal expansion, ice-melt fingerprints, circulation shifts cause regional sea-level trends to diverge.
Current Difference
Pacific mean sea level is ~20–40 cm *higher* than Atlantic at the Panama Canal—a key reason the canal needs locks.
Takeaway
Sea level is a dynamic, spatially variable field—not a universal constant.