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Localized thermosphere ionization events during the high-speed stream interval of 29 April to 5 May 2011

机译:局部热电离层电离事件期间4月29日到5的高速流间隔2011年5月

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We analyze localized ionospheric-thermospheric (IT) events in response to external driving by a high-speed stream (HSS) during the ascending phase of the Solar Cycle 24. The HSS event occurred from ~ 29 April to 5 May, 2011. The HSS itself (and not the associated corotating interaction region) caused a moderate geomagnetic storm with peak SYM-H =-55 nT and prolonged auroral activity. We analyze TIMED (Thermosphere-Ionosphere-Mesosphere Energetics and Dynamics)/SABER (Sounding of the Atmosphere using Broadband Emission Radiometry) measurements of nitric oxide (NO) cooling emission during the interval as a measure of thermospheric response to auroral heating. We identify several local cooling emission (LCE) events in high to subauroral latitudes. Individual cooling emission profiles during these LCE events are enhanced at ionospheric E layer altitudes. For the first time, we present electron density profiles in the vicinity of the LCE events using collocated COSMIC (Constellation Observing System for Meteorology, Ionosphere and Climate) radio occultation (RO) measurements. Measurements at local nighttime show the formation of an enhanced E layer (about 2.5 times increase over the undisturbed value) at ≥100 km altitude. Daytime electron density profiles show relatively smaller enhancements in the E layer. We suggest that the IT response is due to additional ionization caused by medium energy electron (>10 keV) precipitation into the subauroral to high-latitude atmosphere associated with geomagnetic activity during the HSS event.
机译:我们分析局部ionospheric-thermospheric(IT)事件响应外部驱动的在提升高速流(HSS)阶段的太阳周期24。发生在5月5日~ 4月29日,2011年。本身(而不是相关的共转交互区域)温和的地磁引起的风暴峰值SYM-H = -55 nT和延长极光活动。(Thermosphere-Ionosphere-Mesosphere能量和动力学)/军刀(测深的气氛使用宽带发射辐射线测定)测量一氧化氮(NO)冷却期间排放时间间隔的测量thermospheric响应极光加热。在高冷却排放(特性)事件subauroral纬度。如冰事件概要文件在这些增强电离层E层的高度。时间,我们目前的电子密度剖面附近的特性使用集中的事件宇宙(星座观测系统气象、电离层和气候)收音机掩星(RO)测量。当地夜间显示一个增强的形成E层(约增加了2.5倍未扰动值)在≥100公里的高度。电子密度剖面显示相对较小增强在E层。它响应是由于额外的电离由于介质能量电子(> 10 keV)降水到subauroral高纬度大气与地磁活动在高速钢的事件。

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