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eastern Pacific El Niño
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eastern Pacific El Niño
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理学
东太平洋厄尔尼诺
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eastern Pacific El Niño
东太平洋厄尔尼诺
海水升温的最大值位于赤道东太平洋冷舌区的现象。其海水增暖中心一般位于Niño3区(南纬5°~北纬5°,西经150°~90°),亦即秘鲁渔民发现的导致渔获量下降的厄尔尼诺现象。简称东太型厄尔尼诺。由于观测记录中20世纪的绝大多数厄尔尼诺都是东太型厄尔尼诺,因此又称“传统型”厄尔尼诺或“冷舌型”厄尔尼诺。
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