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赤道上升流
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赤道上升流
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理学
赤道上升流
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equatorial upwelling
赤道上升流
出现在赤道太平洋和赤道大西洋次表层到表层的稳定的海水铅直上升运动现象。海洋上升流,在热带海洋-大气相互作用中充当重要角色。
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