从地面FTIR测量中远程监测云参数

J. Thériault, L. Bissonnette, G. Roy
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引用次数: 0

摘要

本文提出了一种利用地面下沉光谱辐射值估算云层温度和透过率的方法。该方法利用臭氧的强发射带,臭氧是探测云层的天然红外辐射源。温度和透过率是由在两个狭窄的光谱通道测量的云天辐射得出的:第一个大约在臭氧带的中心,第二个在带外。云的参数是通过求解一个方程组得到的,这个方程组需要输入从激光雷达回波中获得的云的高度和厚度的估计值,以及大气的温度和湿度剖面。在实验光谱上进行的验证测试表明,该方法在与激光雷达测量时间一致的光谱测量中具有典型的温度误差小于2 K的准确性。最后,对该方法的主要局限性进行了识别和分析。
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Remote monitoring of cloud parameters from ground-based FTIR measurements
In this paper a method for the evaluation of cloud temperature and transmittance from ground-based measurements of the downwelling spectral radiance is proposed. The method uses the strong emission band of ozone at , which constitutes a natural source of IR radiation for probing clouds. Temperature and transmittance are derived from the cloudy-sky radiance measured in two narrow spectral channels: the first one is approximately at the centre of the ozone band at and the second one is off the band at . The cloud parameters are found by solving a system of equations requiring, as input, an estimate of the cloud height and thickness obtained from lidar returns, and of atmospheric temperature and humidity profiles. The validation tests performed on experimental spectra demonstrate the accuracy of the method with typical temperature errors smaller than 2 K for the spectral measurements coincident in time with the lidar measurements. Finally, the main sources of limitations to the method are identified and analysed.
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