Carlon H R
Appl Opt. 1971 Oct 1;10(10):2297-303. doi: 10.1364/AO.10.002297.
An equation modeling ir aerosol emission is presented with experimental data and spectra of low temperature steam from laboratory radiometric measurements. The equation, for the 8-13-micro ir continuum, predicts emissions for traces of liquid water aerosol comparable to those from Elsasser's equation attributed to water vapor. Several curves compare water absorptivity coefficients in the liquid and vapor phases and as applied to atmospheric measurements at the 10.6-micro CO(2) laser wavelength. Results indicate that water aerosols can account for major changes in radiance, even through apparently clear atmospheres. Ice crystals, by implication, represent another fertile field for study as absorbers and emitters.
通过实验室辐射测量得到的低温蒸汽实验数据和光谱,给出了一个模拟红外气溶胶发射的方程。对于8 - 13微米的红外连续谱,该方程预测液态水气溶胶痕量的发射与埃尔萨瑟方程归因于水蒸气的发射相当。几条曲线比较了液相和气相中的水吸收系数,并应用于10.6微米二氧化碳激光波长的大气测量。结果表明,即使在看似晴朗的大气中,水气溶胶也可导致辐射率的主要变化。由此推断,冰晶作为吸收体和发射体代表了另一个值得研究的丰富领域。