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An EJ-Nifie-is a temporary change in the climate of the Pacific Ocean, in the region around the equator. You can see its effects in both the ocean and atmosphere, generally in Northern Hemisphere winter. Typically, the ocean surface warms up by a few degrees Celsius. At the same time, the place where hefty thunderstorms occur on the equator moves eastward. Al-though those might seem like small differences, it nevertheless can have big effects on the world's climate.
What causes it?
Usually, the wind blows strongly from east to west along the equator in the Pacific. This actually piles up water (about half a meter's worth) in the western part of the Pacific. In the eastern part, deeper water (which is colder than the sun- warmed surface water) gets pulled up from below to replace the water pushed west. So, the normal situation is warm water in the west, cold in the east.
In an El Nino, the winds pushing that water around get weaker. As a result, some of the warm water piled up in the west slumps back down to the east, and not as much cold water gets pulled up from below. Both these tend to make the water in the eastern Pacific warmer, which is one of the hallmarks of an El Nino.
But it doesn't stop there. The warmer ocean then affects the winds — it makes the winds weaker! So if the winds get weaker, then the ocean gets warmer, which makes the winds get weaker, which makes the ocean get warmer. . . This is called a positive feedback, and is what makes an El Nino grow.
So what makes it stop growing?
The ocean is full of waves, but you might not know how many kinds of waves there are. There's one called a Rossby wave that is quite unlike the waves you see when you visit the beach. It is more like a distant cousin to a tidal wave. The difference is that a tidal wave goes very quickly, with all the water moving pretty much in the same direction. In a Rossby wave, the upper part of the ocean, say the top 100 meters or so, will be leisurely sliding one way, while the lower part, starting at 100 meters and going on down, will be slowly moving the other way. After a while they switch directions. Everything happens very slowly and inside the ocean, and you can't even see them on the surface. These things are so slow; they can take months or years to cross the oceans. If you had the patience to sit there while one was going by, you'd hardly notice it; the water would be moving 100 times slower than walking speed. But they are large, hundreds or thousands of kilometers in length (not height! Remember, you can hardly see them on the surface),Cartier 14K Yellow Gold Plated Love Ring with Diamond, so they can have an effect on things. Another wave you rarely hear about is called a Kelvin wave, and it had some characteristics in common with Ross by waves, but is somewhat faster than and can only exist closer to the equator (say, within about 5 degrees of latitude around the equator).
El Nines often start with a Kelvin wave propagating from the western Pacific over towards South America. Perhaps you saw, on the TV news, the movie (produced by JPL) for the Elmina of 1997/98? It showed a whitish blob (indicating a sea level some centimeters higher than usual) moving along the equator from Australia to South America. That is one of the hallmarks of a Kelvin wave, the early part of the El Nino process.
When an El Nino gets going in the middle or eastern part of the Pacific, it creates Ross by waves that drift slowly towards Southeast Asia. After several months of travelling, they finally get near the coast and reflect back. The changes in interior ocean temperature that these waves carry with it "cancel out" the original temperature changes that made the El Ni?o in the first place. The main point is that it shuts off when these funny interior-ocean waves travel all the way over to the coast of Asia, get reflected,engagement rings Cartier, and travel back, a process that can take many months.
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