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Statistical climatology of mid-latitude mesospheric summer echoes characterised by OSWIN (Ostsee-Wind) radar observations

机译:以OSWIN(Ostsee-Wind)雷达观测为特征的中纬度中层夏季回波的统计气候学

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Mid-latitude mesospheric summer echoes (MSEs) appear in radar observations during summer months. The geophysical factors controlling the formation of MSEs include solar and energetic particle ionisation, neutral temperature, turbulence, and meridional transport. A total of 12?years of summer months observations with the OSWIN (Ostsee-Wind) radar in Kühlungsborn, Germany, have been analysed to detect MSE events and to analyse statistical connections to these controlling factors. A more sensitive and consistent method for deriving signal-to-noise ratio has been utilised. Daily and monthly composite analysis demonstrates strong daytime preference and early summer seasonal preference for MSEs. The statistical results are not entirely conclusive due to the low-occurrence rates of MSEs. Nevertheless, it is demonstrated that the meridional transport from colder high-latitude summer mesosphere is the important controlling factor, while no clear connection to geomagnetic and solar activity is found.
机译:在夏季月份,中纬度中层夏季回波(MSE)出现在雷达观测中。控制MSE形成的地球物理因素包括太阳和高能粒子电离,中性温度,湍流和子午运输。为了分析MSE事件并分析了与这些控制因素的统计联系,对在德国库伦斯博恩(Kühlungsborn)的OSWIN(Ostsee-Wind)雷达进行的总共12年的观测进行了分析。已经采用了一种更灵敏和一致的推导信噪比的方法。每日和每月的综合分析表明,MSE的白天偏好和夏季初季节偏好强烈。由于MSE的发生率较低,因此统计结果并不完全具有决定性。然而,事实证明,来自较冷的高纬度夏季中层大气的子午线传输是重要的控制因素,而没有发现与地磁和太阳活动的明确联系。

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