Figure 4
From: Impact of deep ocean mixing on the climatic mean state in the Southern Ocean
Sensitivity of ocean hydrography, global MOC, deep convection in the Southern Ocean on deep ocean mixing. (a) Pacific zonal-mean differences of temperature (TED minus CTRL). Values in CTRL are denoted by contours. (b) Same as in (a), but for salinity. (c,d) Global overturning streamfunction. (e,f) Wintertime mixed layer depth which is defined as the depth where the density is higher than that at the sea surface by 0.125 kg m−3. This figure was prepared with GFD-Dennou Common Library version 7.1 (Free Software - http://www.gfd-dennou.org/library/dcl/LICENSE).
