The Costa Rica Coastal Current, eddies and wind forcing in the Gulf of Tehuantepec, Southern Mexican Pacific
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Dynamic structure and atmospheric tropical conditions compared to AVISO images.

Mesoscale eddies on summer resembled those of winter but wind was mainly zonal.

Largest size mesoscale eddies originated outside the Gulf of Tehuantepec.

Water with CRCC characteristics circulated along the eddies edges.

Eddies allow eastern and western flows convergence in front of Puerto Angel.

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