Abstract
Figure 2. Difference between decadal mean AOU (mmol/kg) in the 1990’s and the 1980’s along the isopycnal surface sq 26.6. (a) Total AOU difference is (b) the sum of AOU anomalies due to biological changes, (c) changes in circulation, and (d) ventilation changes. The decadal AOU difference is nearly equal but opposite of the total decadal O2 change, since thermodynamically driven O2 changes are negligible. Contours are shown at intervals of 5 mmol/kg, with dashed lines indicating negative AOU changes. See color version of this figure in the HTML. GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L17610, doi:10.1029/2005GL024471, 2005
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