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Patrick Rafter
oceanandclimate.bsky.social
did:plc:w3z37ar3a4f3osrslxa6tvqc
We argue that this reduced eastern equatorial Pacific stratification during the warm Pliocene makes sense when considering that: (1) subsurface tropical waters originate at higher latitudes and (2) global warming leads to *more* warming at high latitudes. Warmer = less dense and more buoyant.
2025-10-03T00:04:02.355Z