Sea surface temperature temperature pattern is when warm water spreads from the west Pacific and the Indian Ocean to the east Pacific. It takes the rain with it, causing extensive drought in the western Pacific and rainfall in the normally dry eastern Pacific. El Niño's warm rush of nutrient-poor tropical water, heated by its eastward passage in the Equatorial Current, replaces the cold, nutrient-rich surface water of the Humboldt Current. When El Niño conditions last for many months, extensive ocean warming and the reduction in Easterly Trade winds limits upwelling of cold nutrient-rich deep water and its economic impact to local fishing for
Pacific Marine Ecozone (CEC) coast, so there is little oceanic water exchanged between the Arctic and Pacific ecozones. The moderating effect of the Pacific Ocean results in a nearly constant year-round temperature in this ecozone. The Alaska Peninsula also inhibits the flow of cold Arctic currents from entering this zone, ensuring that throughout its extent, there is little variation in temperature. In fact, there is little exchange of oceanic waters between the Pacific Ocean and the Arctic Ocean. Ice forms here infrequently, and only in its northern areas in the Bering Sea and the Sea of Okhotsk. Pacific Marine Ecozone (CEC) The Pacific Marine