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Amplitudes and phases of the diurnal and semidiurnal tide observed in mesospheric OH(3,1) emissions over Maynooth, Ireland

机译:在爱尔兰Maynooth上的中层OH(3,1)排放中观测到的日潮和半日潮的振幅和相位

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摘要

Spectra of the mesospheric OH(3,1) emission have been recorded by an FTIR spectrometer at Maynooth (53.2 degrees N, 6.4 degrees W), of Ireland on all suitable nights during the period December 1992 to July 1995. A total of 370 nights observations have been obtained. Each spectrum is acquired in a five minute integration period, and has been analyzed to yield a value of rotational temperature and brightness associated with the (3,1) band. Each of these measurements has been normalized to the mean value for the particular night on which it was recorded in an effort to extract the amplitude and phase of the variations. The normalized data have been binned at half-hourly intervals for each month so as to minimize the contribution to the variations from gravity waves and short period planetary scale oscillations. Harmonic analysis has been performed to determine an amplitude and a phase of both the diurnal and semidiurnal oscillations for each month in the period under study. The results of this investigation are presented and they are compared with the predictions of the theoretical model of Forbes and Gillette.
机译:1992年12月至1995年7月期间,在爱尔兰所有合适的夜晚,FTIR光谱仪在爱尔兰的Maynooth(北纬53.2度,北纬6.4度)上记录了中层OH(3,1)的发射光谱。已经获得观察。每个光谱在五分钟的积分时间内获取,并已进行分析以产生与(3,1)波段相关的旋转温度和亮度值。这些测量值中的每一个都已标准化为记录有记录的特定夜晚的平均值,以提取变化的幅度和相位。归一化后的数据每个月半小时间隔一次,以使重力波和短期行星尺度振荡对变化的贡献最小。已进行谐波分析,以确定研究期间每个月的昼夜和半日振荡的幅度和相位。介绍了这项研究的结果,并将其与《福布斯》和吉列的理论模型的预测进行了比较。

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