射电望远镜安装在月球背面就可以探测到那些无法在地球表面被检测到的长波，因为它们都被地球大气层的最外层吸收了。
A lunar-based radio telescope would be able to detect long wavelengths that cannot be sensed on Earth because they are absorbed by the outermost layers of the planet's atmosphere.
结果表明：形成大雾的主要原因是大气层结稳定，水汽充沛，地面的长波辐射冷却；
The results showed that longwave radiative cooling is very important for the formation of the fog in addiation to steady atmospheric stratification and plenty of moisture.
利用带模式方法计算了低层大气的长波冷却率。
In this paper, we use the band model to calculate the atmospheric long-wave cooling rates.
结果表明大气中被激发出的长波扰动最初主要是从基本状态的层结不均匀性中得到能量，然后可从波的相互作用中获取能量。
The results show that the excited long wave disturbance could first obtain energy from the stratified heterogeneity of basic state, then from the interactions among non-linear waves.
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。
Increased cloud also blocks the atmospheric window and returns additional long-wave radiation to the ground.
研究表明，云凝结量的次网格水平分布对地面接收的短波辐射和大气顶出射长波辐射通量有明显影响，但短波辐射和长波辐射对云结构的敏感区域有所不同。
Results show that sub-grid distribution of cloud condensate has obvious effect on downwelling shortwave radiation and out-going longwave radiation, with different sensitive domains from each other.
该装置可以保护长波不会被星球最外面的大气层吸收。
The device could protect long wavelength from being absorbed by the outermost layers of the planet's atmosphere.
当然，大气层中一种或种这些气体的变化会影响被截留在温室内的热量和红外长波，从而决定了全球的气候。
Changes in atmospheric levels of either or both of these gases would, of course, affect the amount of heat or long-wave infrared trapped within the greenhouse and thus determine global climate.
结果表明：在太阳反射波段，观测角的影响有很强的波段特性，大气散射作用较强的短波长波段与大气气体强吸收波段是这种影响的敏感波段；
The results show that there are spectral properties about this effect, it is sensitive in the strong scattering regions and the major absorption channels by atmosphere;
大气逆辐射在东北冷区最明显，在黄土高原区最弱；地表长波辐射在西北干旱区最强而在东北冷区最弱。
The downward long-wave radiation is strongest in the cold region and weakest in the Loess Plateau while the upward long-wave radiation is obvious in the arid region and weak in the cold region.
大气逆辐射在东北冷区最明显，在黄土高原区最弱；地表长波辐射在西北干旱区最强而在东北冷区最弱。
The downward long-wave radiation is strongest in the cold region and weakest in the Loess Plateau while the upward long-wave radiation is obvious in the arid region and weak in the cold region.
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