* an atmos circulation in the equatorial regions of the pacific ocean
* warmer water in the western Pacific → causing pow-p, warmer air
* cooler ocean water in the east pacific → causing high-p, cooler air
* winds blow surface ocean water westward (increase sea lvl). cool deep ocean water wells-up along the west coast of South america bringing deep, nutrient-rich seawater to the surface, allowing fish pop to thrive