亚暴周期中极光发射高度的变化:LAMP 火箭实验期间的立体光学观测

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2024-11-12 DOI:10.1029/2024JA033036
K. Hosokawa, Y. Miyoshi, M. Mcharg, V. Ledvina, D. Hampton, M. Lessard, M. Shumko, K. Asamura, T. Sakanoi, T. Mitani, T. Namekawa, M. Nosé, Y. Ogawa, A. Jaynes, A. Halford
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摘要

我们结合 2022 年 3 月 5 日在阿拉斯加进行的 LAMP 探空火箭实验中获得的多处全天空照相机的数据,估算了极光的高度。在火箭发射窗口期间,三台高速全天空照相机在紧靠火箭轨迹下方的三个站点工作:扑克平地、维尼蒂和育空堡。全天空照相机捕捉的全天空图像的时间分辨率为 100 赫兹(育空堡为 80 赫兹)。确定高度的方法是基于对威尼蒂和扑克平的全天空照相机所获得的光学强度时间序列的分析,这些时间序列覆盖了火箭轨迹的下射程区域。结果发现,火箭实验期间脉冲极光的估计高度与利用光发射模型现场观测析出电子得出的高度是一致的,这证实了利用时间序列进行相关分析得出发射高度的可行性。在亚暴开始膨胀后,极光的估计高度有所下降,在恢复阶段的脉动极光间歇期,极光的估计高度略低于 100 公里。特别是,在极光形式从离散型向弥漫型过渡期间,极光发射迅速而短暂地降低到 90 公里左右。这一结果表明,在极光亚暴的扩展阶段开始后不久,存在着一个导致更强电子沉淀的过程。
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Variation of the Altitude of Auroral Emission During a Substorm Cycle: Stereoscopic Optical Observations During the LAMP Rocket Experiment

We estimated the altitude of aurora by combining data from all-sky cameras at multiple places which were obtained during the LAMP sounding rocket experiment in Alaska on 5 March 2022. During the launch window of the rocket, three high-speed all-sky cameras were operative at three stations immediately below the trajectory of the rocket: Poker Flat, Venetie and Fort Yukon. The all-sky cameras captured all-sky images with a temporal resolution of 100 Hz (80 Hz for the Fort Yukon case). The method of altitude determination is based on analyses of time-series of the optical intensity obtained from the all-sky cameras in Venetie and Poker Flat covering the downrange area of the rocket trajectory. The estimated altitude of pulsating aurora during the rocket experiment was found to be consistent with that derived from the in-situ observation of precipitating electrons with a model of optical emission, which confirms the feasibility of deriving the emission altitude through correlation analyses using time-series. The estimated altitude of aurora decreased after the expansion onset of the substorm and stayed slightly below 100 km during the interval of pulsating aurora in the recovery phase. In particular, prompt and brief lowering of the auroral emission, well down to around 90 km, was detected during a transition of auroral form from discrete to diffuse which occurred ∼10 min after the onset. This result implies an existence of a process causing harder electron precipitation operative soon after the start of the expansion phase of auroral substorm.

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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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