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1. 河南科技大学车辆与交通工程学院
2. 上海理工大学能源与动力工程学院
Published:2018
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[1]高凤玲,崔国民.温室效应与地表辐射耦合关系的影响分析[J],2018,35(03):295-300.
[1]高凤玲,崔国民.温室效应与地表辐射耦合关系的影响分析[J],2018,35(03):295-300. DOI: 10.13568/j.cnki.651094.2018.03.008.
DOI:10.13568/j.cnki.651094.2018.03.008.
通过利用一维辐射传递方程及LBLRTM逐线积分模式建立计算模型
本文对地表温度变化所引起的发射能量光谱迁移对温室效应的影响进行了分析.结果表明:地表温度升高会使温室效应增强
而这温度增强效应来自于二个机制:一是地表发射能量改变所引起的强度变化分量;二是辐射能量的光谱迁移所造成的光谱变化分量.强度变化分量始终为正
对温室效应总是起强化作用
而光谱变化分量则根据地表的发射温度以及温室气体的主要吸收带位置有可能为负值
从而对温室效应起削弱作用;极地地区
H_2O与CO2两种主要温室气体的光谱变化分量对温室效应的弱化作用变得很小
因此
在一定程度上对于极地地区的明显温升做出了贡献.
By one-dimensional radiation transfer model
the influence of earth emission spectral characteristics on greenhouse effect was analyzed. The results showed that greenhouse effect will be enhanced with rising temperature by the comprehensive effects of two factors
i.e. the ‘radiation intensity component'(RIC) and the ‘spectral absorption component'(SAC). The RIC always enhances greenhouse effect
while the SAC
as a result of the spectral shift of the earth radiant energy
can enhance or weaken greenhouse effect depending on the positive or negative total SAC integrated over the entire spectral region; in polar region
the weakening influence of SAC from H_2O and CO2 is small
therefore
the temperature rise in polar region is more higher than other regions on the earth.
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