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

<table>The simulated SST in Nino3.4 region from 1950 to 2006 (Blue) forced by NCEP atmospheric forcing and simulated SST from 2001 to 2050 (red) forced by IPCC-AR4 SERS A1B atmospheric forcing using HYCOM model.</table>

Advances in Meteorology

fig5

Figure 5

Figure 5: Dynamic Downscaling of the Impact of Climate Change on the Ocean Circulation in the Galápagos Archipelago 