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- The Pacific Ocean off the coast of Ecuador, Peru, and Chile experiences cooler waters due to the westward movement of warmer waters caused by the warm trade winds1. This process is known as upwelling. The Humboldt current has a considerable cooling influence on the climate of Chile, Peru, and Ecuador2. During the 1988-89 La Niña event, coastal sea-surface temperatures near Ecuador and Peru dropped nearly 4 degrees Celsius (7 degrees Fahrenheit)3. In June 2021, the subsurface cold water from the off-equatorial regions intruded into the equatorial regions between approximately 115°–125° W, interrupting the eastward propagation of warm water along the thermocline4.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.Due to the warm trade winds, the sea surface is normally about 0.5 meter (1.5 feet) higher and 7.2° C (12.96° F) warmer in Indonesia than Ecuador. The westward movement of warmer waters causes cooler waters to rise up toward the surface on the coasts of Ecuador, Peru, and Chile. This process is known as upwelling.www.nationalgeographic.org/encyclopedia/el-nino/The Humboldt has a considerable cooling influence on the climate of Chile, Peru and Ecuador. It is also largely responsible for the aridity of Atacama Desert in northern Chile and coastal areas of Peru and also of the aridity of southern Ecuador.en.wikipedia.org/wiki/Humboldt_CurrentCoastal sea-surface temperatures near Ecuador and Peru dropped nearly 4 degrees Celsius (7 degrees Fahrenheit) during the 1988-89 La Niña event.www.nationalgeographic.org/encyclopedia/la-nina/The turning point of the second-year cooling event occurred in June 2021 when the subsurface cold water from the off-equatorial regions intruded into the equatorial regions between approximately 115°–125° W. This interrupted the eastward propagation of warm water along the thermocline.www.mdpi.com/2077-1312/10/11/1667
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