Dynamic Downscaling of the Impact of Climate Change on the Ocean Circulation in the Galápagos Archipelago

<table class="table-group" width="800px"><tr class="fig-image" id="a"><td><img alt="837432.fig.0020a" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.0020a.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(a) </b>EUC volume flux at 140°W</td></tr></table></td></tr><tr class="fig-image" id="b"><td><img alt="837432.fig.0020b" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.0020b.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(b) </b>SEC volume flux at 140°W</td></tr></table></td></tr><tr class="fig-image" id="c"><td><img alt="837432.fig.0020c" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.0020c.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(c) </b>EUC volume flux at 110°W</td></tr></table></td></tr><tr class="fig-image" id="d"><td><img alt="837432.fig.0020d" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.0020d.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(d) </b>SEC volume flux at 110°W</td></tr></table></td></tr></table>

<table>The compared model and observational EUC (SEC) volume flux transport at 140°W and 110°W, respectively.</table>

Advances in Meteorology

fig20

Figure 20

Figure 20: Dynamic Downscaling of the Impact of Climate Change on the Ocean Circulation in the Galápagos Archipelago 