Wave activity of the mesosphere in the planetary wave range according to OH (3-1) emission observations at Maimaga and Tiksi stations for 2015–2020

V. Sivtseva, P. Ammosov, G. Gavrilyeva, A. Ammosova, I. Koltovskoi
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Abstract

The article compares the interannual variability of the atmosphere at the OH glow height, which can be associated with planetary wave propagation, at stations spaced in latitude. As a characteristic reflecting planetary wave activity we consider standard deviations of the average overnight temperature σpw from its monthly average after taking into account the seasonal variation. Joint mesopause temperature measurements at high latitudes at two optical stations Maimaga (63.04° N, 129.51° E) and Tiksi (71.58° N, 128.77° E) began in 2015. The stations are equipped with identical Shamrock (Andor) high image quality infrared spectrographs for registration of OH (3-1) in the near infrared region (~1.5 μm). The main result of studying the planetary wave activity during the 5-year period of simultaneous observations is that at Tiksi station it slightly (by about 1–2 K) exceeds that at Maimaga station. In average annual activity fluctuations, the presence of quasi-biennial oscillations is traced.
2015-2020年Maimaga站和Tiksi站OH(3-1)发射观测资料在行星波范围内的中间层波活动
本文比较了以纬度为间隔的观测站在与行星波传播有关的OH辉光高度上的大气年际变化。作为反映行星波活动的特征,我们考虑了季节变化后平均夜间温度σpw与月平均值的标准差。2015年开始在Maimaga(63.04°N, 129.51°E)和Tiksi(71.58°N, 128.77°E)两个光学站在高纬度地区联合测量中流层温度。台站配备相同的三叶草(Andor)高成像质量红外光谱仪,用于在近红外区域(~1.5 μm)登记OH(3-1)。在5年同步观测期间研究行星波活动的主要结果是,Tiksi站的行星波活动略超过Maimaga站(约1-2 K)。在平均年活动波动中,可以追踪到准两年振荡的存在。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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