A new CVP-funded modeling study shows that North Atlantic cooling is largely explained by atmospheric processes, rather than a slowdown in ocean circulation.

New data analysis of palaeoceanographic proxies leave scientists with more questions about changes in AMOC.

New study expands the understanding of contemporary decadal variability in the AMOC.

This new study aims to advance decadal prediction models by exploring regionally-dependent coupled sea-surface dynamics at work in the Atlantic and Pacific in initialized prediction ensembles.

Research supported by CPO's Climate Observation Division outlines new facts on the dynamics controlling Atlantic meridional overturning circulation (MOC) variability and highlights some of the unexpected interplay between the density variations in the deep portions of the western region and the direct wind forcing across the basin.