The non-LTE correction to the vibrational component of the internal partition sum for atmospheric calculations

被引:21
作者
Edwards, DP
Lopez-Puertas, M
Gamache, RR
机构
[1] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[2] CSIC, Inst Astrofis Andalucia, E-18080 Granada, Spain
[3] Univ Lowell, Dept Environm Earth & Atmospher Sci, Lowell, MA 01854 USA
关键词
D O I
10.1016/S0022-4073(97)00125-8
中图分类号
O43 [光学];
学科分类号
070207 ; 0803 ;
摘要
In this paper, we develop the theoretical basis for the non-local thermodynamic equilibrium (non-LTE) correction to the vibrational component of the internal partition sum Q(v), and we show how this correction enters into the radiative transfer calculation for a limb-viewing radiometer. The importance of the non-LTE correction to Q(v) depends, for the most part, on the degree to which the lowest vibrational state of the molecule is in non-LTE for a given altitude, since it is this vibration that contributes most to the partition sum. The affect on high-altitude emission depends on the principle excitation mechanism of the radiating molecule, and we compare CO2 and O-3. In the case of CO2, to first order, the high-altitude radiance measured by a limb-viewing radiometer is dependent on the value of the inverse of the partition sum in the region just above the tangent point. We have shown that in the case of the high-altitude temperature sounding channel of the High Resolution Dynamics Limb Sounder (HIRDLS) the non-LTE correction can result in a difference in calculated radiance of some 30% at 130 km. This suggests that the non-LTE correction to Q(v) is an important consideration for high-altitude non-LTE radiative transfer models. (C) 1998 Elsevier Science Ltd. All rights reserved.
引用
收藏
页码:423 / 436
页数:14
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