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

<table>Vertical sections of zonal current (<svg height="16.049999" id="M9" style="vertical-align:-0.16379pt" version="1.1" viewbox="0 0 36.4375 16.049999" width="36.4375" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
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<g transform="matrix(.012,-0,0,-.012,23.05,7.613)"><path d="M535 230h-483v50h483v-50z" id="x2212"></path></g><g transform="matrix(.012,-0,0,-.012,30.035,7.613)"><path d="M384 0h-275v27q67 5 81.5 18.5t14.5 68.5v385q0 38 -7.5 47.5t-40.5 10.5l-48 2v24q85 15 178 52v-521q0 -55 14.5 -68.5t82.5 -18.5v-27z" id="x31"></path></g>
</svg>) along 1°S, 0.5°S equator and 0.5°N for the upper 200 m around the GMR in Dec–Feb 2014 El Niño event.</table>

Advances in Meteorology

fig16

Figure 16

Figure 16: Dynamic Downscaling of the Impact of Climate Change on the Ocean Circulation in the Galápagos Archipelago 