Hovmoeller plot of the anomalous overturning transport at 508N

Density-space overturning streamfunction at (a) 1° and (b) 1 ⁄6°.

PDF) Transient vs. Equilibrium Response of the Ocean's Overturning Circulation to Warming

Louis-Philippe NADEAU, Professor, PhD, Université du Québec à Rimouski UQAR, Rimouski, uqar, Institut des Sciences de la Mer de Rimouski (ISMER)

The time-mean surface density in years 35-40 of the 1° (black) and 1

Louis-Philippe NADEAU, Professor, PhD, Université du Québec à Rimouski UQAR, Rimouski, uqar, Institut des Sciences de la Mer de Rimouski (ISMER)

Annual mean meridional energy transport (PW) in the atmosphere in

Louis-Philippe NADEAU, Professor, PhD, Université du Québec à Rimouski UQAR, Rimouski, uqar, Institut des Sciences de la Mer de Rimouski (ISMER)

Left, top) the cumulative heat uptake by the ocean after 100y in our

PDF) Transient vs. Equilibrium Response of the Ocean's Overturning Circulation to Warming

top) Surface velocity variance with strong winds and (bottom) the

The time-mean surface density in years 35-40 of the 1° (black) and 1

Response to a sudden atmospheric warming in the idealized ocean-ice GCM

The time-mean surface density in years 35-40 of the 1° (black) and 1

Malte F. Jansen's research works University of Chicago, IL (UC) and other places

Arctic sea ice thickness distribution and changes in the late 20th