As the air descends in to the low point of the atmosphericwave, 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。
2
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。
3
In this paper, we use the band model to calculate the atmosphericlong-wave cooling rates.