首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Photometric observations of 630.0-nm 01 and 427.8-nm N_2~+ emission from South Pole and McMurdo Stations during winter: Analysis of temporal variations spanning minutes to hourly timescales
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Photometric observations of 630.0-nm 01 and 427.8-nm N_2~+ emission from South Pole and McMurdo Stations during winter: Analysis of temporal variations spanning minutes to hourly timescales

机译:冬季南极站和麦克默多站630.0-nm 01和427.8-nm N_2〜+发射的光度观测:分析从几分钟到每小时时间尺度的时间变化

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摘要

Time series analysis of zenith-viewing, wide field-of-view photometer measurements of thermospheric OI 630.0-nm and N_2~+ 427.8-nm emissions taken simultaneously from South Pole station (90°S geographic) and from McMurdo station (78°S geographic) during the austral winter months of 2003, 2004, and 2005 are presented. The high sampling rate and continuous, extended duration of measurements at both locations allow for the analysis of phenomena with periods spanning the order of minutes to hours. It is shown that high frequency variations (i.e., with periods of order 1 and 10 min) are often observed at both sites which may be, as supported by colocated magnetometer instrumentation, related to periodic injection of plasma associated with magnetospheric pulsations or their generating processes. We also show that oscillations with periods on the order of 1 h are evident in the power spectrum from both South Pole and McMurdo at both altitudes and emissions and are highly variable. The observations of 12-, 8-, 6-, 4.8-, and 4- h oscillations are believed to be due to daily sampling of the auroral zone emissions along with potential moonlight contamination. Other observed periods with order 1 h require further study but are likely due to auroral poleward boundary intensifications. The approach presented herein serves as a means to quickly identify time periods of geophysical activity which will be useful in a future analysis of a much greater, extended climatology of the various spectral features, e.g., a 2 decade survey of poleward moving auroral form events currently in progress. The results herein also assist in providing context to the analysis of synoptic space weather events with photometers and provide support for recently reported auroral intensity variations in the Pc5 band.
机译:从南极站(地理坐标为90°S)和麦克默多站(地理坐标为78°S)同时采集的热球OI 630.0-nm和N_2〜+ 427.8-nm发射的天顶观测,宽视场光度计测量的时间序列分析展示了2003、2004和2005年冬季南方的月份)。两个位置的高采样率和连续,延长的测量持续时间允许对现象进行分析,周期范围从几分钟到几小时不等。结果表明,在两个位置上经常观察到高频变化(即,周期为1和10分钟),这可能是由共置磁力计仪器支持的,这与周期性注入与磁层脉动有关的等离子体或其产生过程有关。我们还表明,在南极和麦克默多的功率谱中,高度和发射处的功率谱中都明显出现了周期为1 h左右的振荡,并且变化很大。据信观察到12、8、6、4.8和4 h振荡是由于每天对极光区排放物以及潜在的月光污染进行采样。其他观察到的1小时左右的周期需要进一步研究,但是可能是由于极光极地边界的加剧。本文介绍的方法是一种快速识别地球物理活动时间段的手段,这将在将来对各种光谱特征的更大范围的扩展气候学进行分析时很有用,例如,目前对极地移动极光形式事件进行的20年调查进行中。本文的结果还有助于为用光度计分析天气天气天气事件提供背景,并为最近报道的Pc5波段极光强度变化提供支持。

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