首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Unusual 5mE region field-aligned irregularities observed from Northern Germany during the magnetic storm of 17 March 2015
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Unusual 5mE region field-aligned irregularities observed from Northern Germany during the magnetic storm of 17 March 2015

机译:不寻常的5我地区field-aligned违规行为观察期间从德国北部2015年3月17磁暴

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Coherent E region echoes were observed during the 17 March 2015 storm at midlatitudes by multistatic wide field of view radars operating in northern Germany. Two of the stations operated in a monostatic configuration, while one link was set in bistatic mode. Interferometry made it feasible to locate the targets. While the radars were built to measure mesospheric winds from specular meteor echoes, the storm was so intense that it allowed them to observe auroral E region echoes for more than 4 h. All stations detected numerous examples of narrow spectra with slow (≈180 m/s) and fast (up to 1600 m/s) Doppler velocities. The target speeds were much faster than the Doppler velocities for the slow narrow echoes (more than 800 m/s versus 180 m/s) but comparable to the observed Doppler shift for the 1500 m/s narrow fast types. The narrow types came from localized horizontal structures 50 to 80 km wide in range. The fast narrow types came from the upper part of the altitudes associated with Farley-Buneman waves. The slow narrow structures were typically from altitudes lower than 100 km. Unexpectedly, the great majority of the echoes associated with more ordinary ion acoustic turbulence had a positive Doppler shift and came from the east. A companion paper uses these new observations to reevaluate the origin of the narrow echoes and of the asymmetry in the counts. Irrespective of the generation mechanisms, our observations indicate that a combination of unusually large electric field and strong precipitation is needed to produce the unusual echoes.
机译:观察在相干E区回声2015年3月17日风暴在情理之中多宽的视野雷达操作在德国北部。在单站配置中,当一个链接设置在收发分置的模式。可行的定位目标。建立衡量中层风镜面流星回声,暴风雨是如此强烈它允许他们观察极光E回声超过4 h。所有电台检测无数的例子窄光谱与缓慢(≈180 m / s)和快速(最高可达1600 m / s)多普勒速度。比多普勒速度缓慢缩小回声(超过800 m / s和180 m / s)与观察到的多普勒频移的1500 m / s狭窄快速类型。从本地化水平结构50到80公里宽范围内。的上部高度相关Farley-Buneman波。通常从海拔低于100公里。出乎意料的,绝大多数的回声与更多的普通离子声波湍流有积极的多普勒频移和来了从东。观察来评估的起源狭窄的回声和不对称的数量。无论生成机制,我们的观察表明的组合异常大的电场和强大需要沉淀产生不寻常的回声。

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