El Niño, A Non-technical Description

Non-technical explanation of the El Niño phenomenon, the El Nino phenomenon is a temporary change of the Pacific climate near the equator. You can see its effect in the ocean and atmosphere, usually in the winter of the Northern Hemisphere. Normally, the sea level gets hot at several degrees Celsius. At the same time, the direction of the heavy thunderstorm on the equator will move east. These may not seem important, but they have a major impact on the world climate.

El Nino is now named El Nededa by a fisherman in Peru in the 17th century. This name is used because this phenomenon tends to reach Christmas. The climate record of the El Nino phenomenon dates back many millions of years and there is evidence that this cycle is found in ice core, deep sea mud, coral, cave and annual rings. In the normal non El Nino phenomenon, the trade wind blows away from South America to the western Pacific Ocean. Because these winds accumulate the warm surface waters of the western Pacific, the ocean off Indonesia is higher than the Pacific Ocean and about 1 to 2 feet (0.3 to 0.6 meters) off Ecuador.

Non-technical explanation of the El Niño phenomenon, the El Nino phenomenon is a temporary change of the Pacific climate near the equator. You can see its effect in the ocean and atmosphere, usually in the winter of the Northern Hemisphere. Normally, the sea level gets hot at several degrees Celsius. At the same time, the direction of the heavy thunderstorm on the equator will move east. - The title of the research paper is a survey on the education of library users at Taiwan University and National College of Technology. According to the research title, we clearly describe the contents of the research and explain accurately. This is because it is easy to show the problem the given title will be discussed in the study. Therefore, it was not difficult for other researchers and scholars to keep track of the view of this research.

El Niño - Southern Oscillation is a single climatic phenomenon which periodically fluctuates between the three stages of neutral, La Niña, El Niño. La Niña and El Niño are the opposite stages, and some changes in the ocean and atmosphere must be made before the event is announced. Typically, the northern flow of the Humboldt current brings relatively cool water from South America to the tropical region along the west coast of South America where it is strengthened by upward flow along the coast of Peru. The trade wind along the equator helps the ocean currents in eastern Pacific to absorb water from the deeper ocean to the surface and keep the surface cool. Due to the influence of the equatorial trade wind, this cold water flows west along the equator and it is slowly heated by the sun.