Extended Data Fig. 7: Perturbed Atlantic overturning stream-function (Sv) at interglacial, intermediate and glacial climate conditions.
From: A salty deep ocean as a prerequisite for glacial termination
Atlantic overturning stream-function (Sv, 106 m3 s−1) in the perturbation experiments representing the average between model years 100-200 for a) interglacial (PIDPERT), b) intermediate (40kaPERT) and c) glacial maximum (LGMPERT) conditions (cf. Fig. 4a). Solid contours indicate clockwise NADW circulation and doted contours anti-clockwise AABW circulation.
