由澳大利亚阿德莱德上空的OH(6-2)排放确定的中间层旋转温度

B.G Hobbs , I.M Reid , P.A Greet
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引用次数: 9

摘要

本文介绍了1993年9月在南澳大利亚阿德莱德附近的巴克兰公园(Buckland Park)野外站(34°38'S, 138°29'E)用OH光谱仪和中频雷达在6个晚上观测到的潮汐样变化。在OH数据中观察到一个突出的半日潮汐样的温度变化,峰对峰的幅度高达40k。温度和风的振幅和相位与半日模式进行比较,数量之间的关系也是如此。此外,还将观测到的温度变化与前人的研究结果进行了比较。关于振幅和相位的绝对值,模型和观测值不同。然而,就相位而言,观察到的数量之间的关系与六个单独夜晚中的四个夜晚的模型以及六个夜晚的平均数据非常吻合。
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Mesospheric rotational temperatures determined from the OH(6-2) emission above Adelaide, Australia

Tide-like variations observed in data from an OH spectrometer and MF radar, co-located at the Buckland Park field station (34°38′S, 138°29′E) near Adelaide, South Australia, over six nights in September 1993 are presented. A prominent semi-diurnal tide-like variation in temperature with a magnitude of up to 40 K peak-to-peak is observed in the OH data. Temperature and wind amplitudes and phases are compared with a semi-diurnal model, as are the relationships between the quantities. In addition, the observed temperature variations are compared with those of previous researchers. With regard to the absolute values of the amplitudes and phases, the model and observations differ. However, the observed relationships between the quantities, in terms of phase, are found to agree well with the model for four of the six individual nights, as well as for data that are the average of the six nights.

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