计算得到的大气水汽斜程吸收和分布。
Calculated slant-path absorption and distribution of atmospheric water vapor.
作者信息
Calfee R F, Gates D M
机构信息
Institute for Telecommunication Sciences and Aeronomy of the Environmental Science Services Administration, National Bureau of Standards, Boulder, Colorado, USA.
出版信息
Appl Opt. 1966 Feb 1;5(2):287-92. doi: 10.1364/AO.5.000287.
PMID:20048832
Abstract
A procedure is described for determining the amount and distribution of water vapor along a slant path through the atmosphere above 13.7 km. A multilayer analysis is used in which the transmittance of each layer is calculated and the accumulative effect obtained at the altitude of observation. The method depends upon the contribution of each line to the absorptance in a finite spectral region.
摘要
本文描述了一种用于确定沿13.7公里以上大气层倾斜路径的水汽含量和分布的方法。采用多层分析法，计算每一层的透过率，并在观测高度得到累积效应。该方法取决于每条谱线在有限光谱区域内对吸收率的贡献。
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