Observations of Strong Range Spread F and Nighttime Ionospheric Enhancement in the Mid-Latitude Region Under Geomagnetically Quiet Conditions

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2024-11-19 DOI:10.1029/2024JA033106
Chunhua Jiang, Rong Tian, Tongxin Liu, Guobin Yang, Hua Shen, Wengeng Huang, Zhengyu Zhao
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Abstract

Spread F is one of most widely observed nighttime ionospheric irregularities by ionosondes in the equatorial, low- and mid-latitude regions. One type of spread F, known as strong range spread F (backscatter echoes beyond the critical frequency of the F2 layer, foF2), has been observed in the equatorial and low-latitude regions but not at middle latitudes. This study reported for the first-time observations of strong range spread F at Zhangye Station (ZHY, Geographical latitude 39.4°N, longitude 100.0°E, Dip Lat 29.6°N) on 29 November 2019 (under quiescent conditions). Observations show that strong range spread F occurred at first during midnight (∼16:30 UT), accompanied with mid-latitude nighttime ionospheric enhancements in foF2 and total electron content (TEC). Then, it becomes more pronounced when ionospheric collapse occurred. The measurements from satellite revealed that there are large opposite temperature and density gradients (temperature decreased sharply from ∼3100 to ∼2500 K, however, electron density increased sharply from ∼0.3 e5 to ∼1.2 e5 cm−3 around Zhangye Station) during this event. Results suggest that mid-latitude strong range spread F might be attributed to temperature gradient instabilities.

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地磁静止条件下中纬度地区强范围展宽 F 和夜间电离层增强的观测结果
扩展 F 是赤道、低纬度和中纬度区域电离层探测仪观测到的最广泛的夜间电离层 不规则现象之一。在赤道和低纬度地区观测到的一种扩展 F 被称为强范围扩展 F(超过 F2 层临界频率 foF2 的反向散射回波),但在中纬度地区没有观测到。本研究首次报道了 2019 年 11 月 29 日(静态条件下)在张掖站(ZHY,地理纬度 39.4°N,东经 100.0°E,浸纬 29.6°N)观测到的强范围扩散 F。观测结果表明,最初在午夜(16:30∼16:30 UT)出现了强范围扩散F,同时伴随着中纬度夜间电离层foF2和电子总含量(TEC)的增强。然后,当电离层发生坍缩时,它变得更加明显。卫星测量结果表明,在这一事件中,存在着较大的相反温度梯度和密度梯度(温度从∼3100 K急剧下降到∼2500 K,但电子密度在张掖站周围从∼0.3 e5急剧增加到∼1.2 e5 cm-3)。结果表明,中纬度强范围扩散F可能是由温度梯度不稳定性引起的。
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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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