As the air descends in to the low point of the atmospheric wave, it touches the ocean surface, causing rough waters, visible here as long, dark vertical lines.
在空气下降到大气波的低点时，与海洋的表面相接触，形成了像漫长、黑暗垂直线条那样，明显的惊涛骇浪。
Increased cloud also blocks the atmospheric window and returns additional long-wave radiation to the ground.
云的增加对大气窗区也起著屏蔽作用，因而使额外的长波辐射返回地面。
In this paper, we use the band model to calculate the atmospheric long-wave cooling rates.
利用带模式方法计算了低层大气的长波冷却率。
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