首页> 外文会议>Tenth Joint International Symposium on Atmospheric and Ocean Optics/Atmospheric Physics Part.II Laser Sensing and Atmospheric Physics; Jun 24-28, 2003; Tomsk, Russia >Measurements of upper mesosphere temperature on the height of night sky emission excitation OH and O2(0-1) in Yakutsk
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Measurements of upper mesosphere temperature on the height of night sky emission excitation OH and O2(0-1) in Yakutsk

机译:雅库茨克夜空发射激发OH和O2(0-1)高度上中层温度的测量

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摘要

The results of the hydroxyl and oxygen molecules rotational temperature measured during two observational seasons 1999-2001 in Maymaga station (φ=63°N; λ=129.50°E) are presented. It is shown that the amplitude of seasonal variation of hydroxyl rotational temperature is greater than the molecular oxygen variation. OH temperatures have been systematically higher the O_2 ones during winter. The abrupt decreasing of the O_2 intensity connected with the springtime transition of the atmospheric circulation process is found in both time series. In first time a change of the temperature vertical gradient sign caused by the mesopause height shifting to the more high (winter) level was shown in the data of August-September 2001. Comparisons of night airglow variations with stratospheric temperature over Yakutsk at the 10 mb height, averaged over the polar cap (latitudes of ≥65°N), is presented. The waves registered in mesosphere by variation of molecular oxygen emission rate are of periods up to ten days, and the envelope of their amplitudes is similar to stratosphere temperature oscillations with a time scale o f approximately 30 days. Such a close association of two different p arameters in the a tmosphere r egions separated in height c an be e xplained by p assage o f large-scale wave disturbances through them.
机译:给出了在Maymaga站的两个观测季节1999-2001年(φ= 63°N;λ= 129.50°E)测得的羟基和氧分子旋转温度的结果。结果表明,羟基旋转温度的季节性变化幅度大于分子氧的变化幅度。冬季,OH的温度总体上高于O_2的温度。在两个时间序列中都发现与大气循环过程的春季转变有关的O_2强度的突然降低。第一次在2001年8月至9月的数据中显示了由更年期高度转变为更高(冬季)水平引起的温度垂直梯度符号的变化。比较了雅库茨克地区10 mb处夜间气辉变化与平流层温度的变化。给出了极帽上的平均高度(纬度≥65°N)。通过改变分子氧释放速率而在中层层中记录的波的周期长达十天,其幅度的包络类似于平流层温度振荡,时间尺度约为30天。在大气层中两个不同的参数在高度上分隔开的这种紧密联系可以通过对它们的大规模波浪干扰的评估来说明。

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