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.006a" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.006a.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(a) </b>Nino3.4 SSTA wavelet power spectrum (1950–2050)</td></tr></table></td></tr><tr class="fig-image" id="b"><td><img alt="837432.fig.006b" src="https://static.hindawi.com/articles/amete/volume-2013/837432/figures/837432.fig.006b.jpg"/></td></tr><tr class="fig-caption"><td align="center"><table><tr><td><b>(b) </b>Spectrum of SSTA in Nino3.4 region</td></tr></table></td></tr></table>

<table>The evolution of the difference of the sea level pressure anomaly (ΔSLP) between East Pacific (80°E-160°E, 5°S-5°N) and West Pacific (160°W-80°W, 5°S-5°N)  and zonal wind stress anomaly in equatorial Pacific (120°E-70°W, 5°S-5°N) since the 20th century from IPCC-AR4IPCC-AR4 data.</table>

Advances in Meteorology

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Figure 6

Figure 6: Dynamic Downscaling of the Impact of Climate Change on the Ocean Circulation in the Galápagos Archipelago 