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Double Coherent Scatter Radars Observations of the Daytime F-Region Irregularities in Low-Latitudes on 29 May 2017

文献类型：期刊论文

作者Hu, Pengfei1; Chen, Gang1; Li, Guozhu2; Yan, Chunxiao1,3; Zhang, Shaodong1; Yang, Guotao3; Li, Yaxian1; He, Zhiqiu1; Jia, Wei1; Zhang, Min1
刊名SPACE WEATHER-THE INTERNATIONAL JOURNAL OF RESEARCH AND APPLICATIONS
出版日期2022-12-01
卷号20期号:12页码:13
关键词F-region irregularity daytime
DOI10.1029/2022SW003272
英文摘要In the morning on 29 May 2017, the Sanya very-high-frequency Radar and the Hainan COherent Scatter Phased Array Radar (HCOPAR) at Fuke were cooperated with similar operating frequencies to investigate the dissipation of the daytime F-region Field-Aligned Irregularities (FAIs). The two radars are located on south and north sides of the Hainan island of China, and the distance between them is about 140 km. The Sanya VHF radar recorded the FAIs between 00:12 and 02:42 UT (07:12 and 09:42 LT), and the FAIs observed by the HCOPAR appeared more than 10 min later at lower altitudes and suffered severe dissipation. The echoes emerged in all the beams simultaneously, and their Doppler velocities were close to zero, implying that the daytime FAIs were traveling along the magnetic field lines downward and northward with almost no zonal velocity. The front and bottom edges of the irregularities decayed earlier, and the parts in the FAIs with steeper density gradient lasted longer. The dissipation mechanism is attributed primarily to the photoionization and diffusing across the geomagnetic field in different period and gradient of the irregularities. Plain Language Summary Equatorial Plasma Bubbles, which cause Field-Aligned Irregularities (FAIs), are widely accepted as a nighttime phenomenon. They usually disappear before sunrise and are rarely recorded by radars during daytime. Especially the dissipation process of the daytime FAIs is seldom reported. The Sanya very-high-frequency radar located on the south of the Hainan Island and the Hainan COherent Scatter Phased Array Radar located on the north observe the daytime FAIs successively. The observation results show that while the daytime FAIs were traveling from Sanya to Fuke, the dissipation process first occurred in the front and bottom edges as well as the regions of the irregularities with small density gradient. The dissipation mechanism for the fossil F-region FAIs traveling along the magnetic field lines under the sun are discussed. This investigation results may deepen our understanding of the dissipation processes in the irregularity and their interaction with the ambient atmosphere.
WOS关键词EQUATORIAL PLASMA BUBBLES ; FIELD-ALIGNED IRREGULARITIES ; SPREAD-F ; TOPSIDE IONOSPHERE ; NEUTRAL WINDS ; EVOLUTION ; STORM ; SCINTILLATION ; TERMINATOR ; SCALE
资助项目National Natural Science Foundation of China[42274197] ; National Natural Science Foundation of China[41722404] ; Foundation of National Key Laboratory of Electromagnetic Environment[JCKY2020210C614240306]
WOS研究方向Astronomy & Astrophysics ; Geochemistry & Geophysics ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000924484400001
出版者AMER GEOPHYSICAL UNION
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Foundation of National Key Laboratory of Electromagnetic Environment ; Foundation of National Key Laboratory of Electromagnetic Environment ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Foundation of National Key Laboratory of Electromagnetic Environment ; Foundation of National Key Laboratory of Electromagnetic Environment ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Foundation of National Key Laboratory of Electromagnetic Environment ; Foundation of National Key Laboratory of Electromagnetic Environment ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Foundation of National Key Laboratory of Electromagnetic Environment ; Foundation of National Key Laboratory of Electromagnetic Environment
源URL[http://ir.iggcas.ac.cn/handle/132A11/106807]  
专题地质与地球物理研究所_中国科学院地球与行星物理重点实验室
通讯作者Chen, Gang
作者单位1.Wuhan Univ, Elect Informat Sch, Wuhan, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Beijing, Peoples R China
3.Chinese Acad Sci, State Key Lab Space Weather, Natl Space Sci Ctr, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Hu, Pengfei,Chen, Gang,Li, Guozhu,et al. Double Coherent Scatter Radars Observations of the Daytime F-Region Irregularities in Low-Latitudes on 29 May 2017[J]. SPACE WEATHER-THE INTERNATIONAL JOURNAL OF RESEARCH AND APPLICATIONS,2022,20(12):13.
APA Hu, Pengfei.,Chen, Gang.,Li, Guozhu.,Yan, Chunxiao.,Zhang, Shaodong.,...&Zhang, Min.(2022).Double Coherent Scatter Radars Observations of the Daytime F-Region Irregularities in Low-Latitudes on 29 May 2017.SPACE WEATHER-THE INTERNATIONAL JOURNAL OF RESEARCH AND APPLICATIONS,20(12),13.
MLA Hu, Pengfei,et al."Double Coherent Scatter Radars Observations of the Daytime F-Region Irregularities in Low-Latitudes on 29 May 2017".SPACE WEATHER-THE INTERNATIONAL JOURNAL OF RESEARCH AND APPLICATIONS 20.12(2022):13.

入库方式： OAI收割

来源：地质与地球物理研究所

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