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.003a" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.003a.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(a) </b>Spectrum of SSTA in Nino3.4 region (Model)</td></tr></table></td></tr><tr class="fig-image" id="b"><td><img alt="837432.fig.003b" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.003b.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(b) </b>Spectrum of SSTA in Nino3.4 region (Obs)</td></tr></table></td></tr></table>

<table>The power spectrum of the SST anomalies in the Nino3 region during 1950–2006 obtained from the (a) model simulation and (b) observation.</table>

Advances in Meteorology

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Figure 3

Figure 3: Dynamic Downscaling of the Impact of Climate Change on the Ocean Circulation in the Galápagos Archipelago 