The El Nino.
As usual, the territorial tropical Pacific or the Pacific tropics are the trade winds East covered regularly. This wind will blow the warm sea surface from the East. (coast of Ecuador and Peru, Chile north) to accumulate in the West (coast of Indonesia and Australia). The atmosphere over the Pacific West is due to evaporation, moisture movement (Glantz 2001) and formations of clouds and rain, the East and southeast of Asia. As well as various countries on an island in the Western Pacific (Figure 1) while east of the Pacific tropics more flow of water at the bottom to the surface and cause ความแห้งแล้งบริเวณ coast of South America. But when the trade winds East is younger than normal. The wind blows the cover on the east side of Papua New Guinea (Papua New Guinea is a island located on the Pacific equatorial area north west of Australia). To change direction from the East is West. Ripple effect under the water brought mass warm water accumulated in the Western Pacific to replace the water cooler to the eastern Pacific. When the mass of warm water has been transported to the East Pacific. The coast of Ecuador () are integrated with the surface of the water. The sea surface area is warmer than normal, and the warm water will gradually expand the area ไปทางตะวันตก to the middle of the ocean. Result in the formation of clouds and rain, which is usually in the sun. The fall of the change in the middle and East (Figure 2) the area has the rain than usual. While the Western Pacific, which had much rain will be less rain and drought.
นิโนเอลAs usual, the territorial tropical Pacific or the Pacific tropics are the trade winds East covered regularly. This wind will blow the warm sea surface from the East. (coast of Ecuador and Peru, Chile north) to accumulate in the West (coast of Indonesia and Australia). The atmosphere over the Pacific West is due to evaporation, moisture movement (Glantz 2001) and formations of clouds and rain, the East and southeast of Asia. As well as various countries on an island in the Western Pacific (Figure 1) while east of the Pacific tropics more flow of water at the bottom to the surface and cause ความแห้งแล้งบริเวณ coast of South America. But when the trade winds East is younger than normal. The wind blows the cover on the east side of Papua New Guinea (Papua New Guinea is a island located on the Pacific equatorial area north west of Australia). To change direction from the East is West. Ripple effect under the water brought mass warm water accumulated in the Western Pacific to replace the water cooler to the eastern Pacific. When the mass of warm water has been transported to the East Pacific. The coast of Ecuador () are integrated with the surface of the water. The sea surface area is warmer than normal, and the warm water will gradually expand the area ไปทางตะวันตก to the middle of the ocean. Result in the formation of clouds and rain, which is usually in the sun. The fall of the change in the middle and East (Figure 2) the area has the rain than usual. While the Western Pacific, which had much rain will be less rain and drought.
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