“大气水循环”的概念、定义、翻译、参考文献-科学参考

大气水循环

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。

单词	大气水循环
释义	大气水循环 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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