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大气逆辐射 [dà qì nì fú shè]
[气象] atmospheric counter radiation
- 季节变化对大气逆辐射分布形势影响不大，而对有效辐射分布的影响较大，可造成高值中心的位移。
The main body of the Plateau represents the low-(high-) value center for downward atmospheric (effective) radiation. - 大气逆辐射与地面长波辐射随大气温度和地表温度变化明显。
The atmospheric counter radiation and terrestrial long-wave radiation change with the air temperature and surface temperature significantly. 3. - 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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