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atmospheric water cycle
释义
atmospheric water cycle
Encyclopedia
理学
大气水循环
释
atmospheric water cycle
大气水循环
地球海陆表面的水分,在太阳辐射和地表热力作用下,通过蒸发(包括冰雪的升华)和植被蒸腾以水蒸气的形式进入大气,在一定条件下(主要通过气流的辐合)抬升,随大气环流在时间空间分布上持续动态变化。在适当的大气热力作用下,水汽发生凝结,受重力作用以液态(降雨)或固态(降雪、雹、霰)形式降落到地面的整个运动过程。
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更新时间:2025/7/26 2:30:53