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Upper mesosphere/ lower thermosphere temperatures from non-LTE modelling of the CRISTA 15μm measurements

机译:来自Crista15μm的非LTE建模的上部叶片/较低的热层温度

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The CRyogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) experiment measured mid-and far-infrared limb spectra during two Shuttle missions in November 1994 and August 1997 from the upper troposphere to the lower thermosphere. From the CO_2 15μm spectra temperatures in the mesosphere and lower thermosphere were derived using a non-LTE model coupled to a line-by-line radiative transfer code. CO_2 and atomic oxygen densities were calculated from the simultaneously recorded 4.3μm (CO_2) and 9.6 μm (ozone) measurements. The retrieved temperatures reveal the very low high latitude summer mesopause temperatures. Zonal structures are found at all altitudes and in the summer hemisphere as well as in the winter hemisphere. The north polar temperature distribution near the mesopause is dominated by a wave 1 structure with some wave 2 contribution. The same pattern is observed in the distribution of polar mesospheric clouds (PMC) which were detected via their thermal emission near 12 μm. The appearance of the PMCs thus verifies the temperatures obtained from the non-LTE modelling. The wave structures extend well into the thermosphere.
机译:大气(Crista)的低温红外光谱仪和望远镜在1994年11月和1997年8月的两台梭式任务中测量了中频和红外肢体光谱,从上层对流层到下热圈。从介于逐行辐射传输代码耦合的非LTE模型导出了介质圈和较低的热圈中的CO_215μm光谱温度。通过同时记录的4.3μm(CO_2)和9.6μm(臭氧)测量来计算CO_2和原子氧密密度。检索到的温度揭示了非常低的高纬度夏季夏季夏季气温。在所有高度和夏季半球和冬季半球中都发现了区间结构。北极代的北极温度分布由波浪1结构主导,具有一些波2的贡献。在极性延长云(PMC)的分布中观察到相同的图案,其通过其热排放接近12μm检测。因此,PMC的外观验证了从非LTE建模获得的温度。波形结构延伸到热圈中。

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