Impacts of Wind Stress Changes on the Global Heat Transport, Baroclinic Instability, and the Thermohaline Circulation

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/2089418/figures/2089418.fig.004a.svgz" name="2089418.fig.004a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Atlantic Ocean</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/2089418/figures/2089418.fig.004b.svgz" name="2089418.fig.004b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Pacific Ocean</td></tr></table>

<div>Annual salt transport zonally averaged (Sv). (a) Atlantic Ocean and (b) Pacific Ocean. Black line: CTR simulation; red line: EQU 50% simulation; and green line: 46°S 50% simulation.</div>

Advances in Meteorology

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Figure 4

Figure 4: Impacts of Wind Stress Changes on the Global Heat Transport, Baroclinic Instability, and the Thermohaline Circulation 