Hovmoeller plot of the anomalous overturning transport at 508N
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Density-space overturning streamfunction at (a) 1° and (b) 1 ⁄6°.
Anomalous air-sea heat flux from an ensemble of 15 CMIP5 experiments
Annual mean meridional energy transport: a total (black), ocean (blue)
Hovmoeller plot of the anomalous overturning transport at 508N
top) A breakdown of the flow of water lighter than 2000 1035.8 kg m 3
Annual mean meridional energy transport (PW) in the atmosphere in
top) A breakdown of the flow of water lighter than 2000 1035.8 kg m 3
Annual mean meridional energy transport (PW) in the atmosphere in
Density anomaly relative to the reference simulation (kg m 23 ; with
PDF) Transient vs. Equilibrium Response of the Ocean's Overturning Circulation to Warming
The time-mean surface density in years 35-40 of the 1° (black) and 1
As in Fig. 1, but showing the response to a uniform 38C surface warming
Arctic sea ice thickness distribution and changes in the late 20th
PDF) Transient vs. Equilibrium Response of the Ocean's Overturning Circulation to Warming
Left, top) the cumulative heat uptake by the ocean after 100y in our
