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.008a.svgz" name="2089418.fig.008a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Atmosphere + Ocean</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/2089418/figures/2089418.fig.008b.svgz" name="2089418.fig.008b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Atlantic Ocean</td></tr><tr class="fig-image" id="c"><td><object data="https://static.hindawi.com/articles/amete/volume-2016/2089418/figures/2089418.fig.008c.svgz" name="2089418.fig.008c" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(c) </b>Pacific Ocean</td></tr></table>

<div>Heat transport zonally averaged (PW). (a) Total heat transport, (b) heat transport in Atlantic Ocean, and (c) heat transport in 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 8

Figure 8: Impacts of Wind Stress Changes on the Global Heat Transport, Baroclinic Instability, and the Thermohaline Circulation 