Resumo: |
One hundred oceanographic stations were occupied in front of Ecuador during september 1995. All the information were treated statically using the method of ”Kriging” to interpolate from this; surface distributions of sea temperature, sea temperature anomalies, air temperature, and atmospheric presion were obtained. These distribution with temperature and salinity profiles showed between normal and cold climatical conditions. Comparing the sea density horizontal distribution and the water mass, with the capture areas distributions of Sardinops sagax, resulted that areas with hight capture had AESS in low quantity and hand too a surface thermocline.
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