Vertical Structural Evolution of Ionospheric Holes Triggered by Rocket Launches Observed by the Sanya Incoherent Scatter Radar

IF 2.9 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2024-11-28 DOI:10.1029/2024JA033171
Linxuan Zhao, Feng Ding, Xinan Yue, Su Xu, Junyi Wang, Yihui Cai, Mingyuan Li, Ning Zhang, Xu Zhou, Yonghui Wang, Jianyong Li, Tian Mao, Qian Song, Bo Xiong, Xiaolin Li, Junhao Luo
{"title":"Vertical Structural Evolution of Ionospheric Holes Triggered by Rocket Launches Observed by the Sanya Incoherent Scatter Radar","authors":"Linxuan Zhao,&nbsp;Feng Ding,&nbsp;Xinan Yue,&nbsp;Su Xu,&nbsp;Junyi Wang,&nbsp;Yihui Cai,&nbsp;Mingyuan Li,&nbsp;Ning Zhang,&nbsp;Xu Zhou,&nbsp;Yonghui Wang,&nbsp;Jianyong Li,&nbsp;Tian Mao,&nbsp;Qian Song,&nbsp;Bo Xiong,&nbsp;Xiaolin Li,&nbsp;Junhao Luo","doi":"10.1029/2024JA033171","DOIUrl":null,"url":null,"abstract":"<p>This article presents observational results of the vertical structural evolution of ionospheric holes during two rocket launches. A combination of observations from the newly built Sanya incoherent scatter radar (SYISR) and Global Navigation Satellite System networks was employed. The vertical structural evolution of two rocket-induced ionospheric holes over the SYISR could be divided into three stages. Firstly, 10–11 min after launch, the holes initially appeared in the topside ionosphere. Then, the holes expanded rapidly toward higher and lower altitudes. At ∼30 min after launch, the holes extended to an altitudinal range of ∼200 km to over 700 km. The maximum depletion altitude was 425 km for the afternoon event and 283 km for the midnight event. Finally, the holes recovered slowly, with faster recovery at higher altitudes. Our work contributes to further understanding the vertical structural evolutionary mechanisms of the ionospheric holes and relevant ionospheric processes.</p>","PeriodicalId":15894,"journal":{"name":"Journal of Geophysical Research: Space Physics","volume":"129 12","pages":""},"PeriodicalIF":2.9000,"publicationDate":"2024-11-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024JA033171","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Space Physics","FirstCategoryId":"89","ListUrlMain":"https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024JA033171","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

This article presents observational results of the vertical structural evolution of ionospheric holes during two rocket launches. A combination of observations from the newly built Sanya incoherent scatter radar (SYISR) and Global Navigation Satellite System networks was employed. The vertical structural evolution of two rocket-induced ionospheric holes over the SYISR could be divided into three stages. Firstly, 10–11 min after launch, the holes initially appeared in the topside ionosphere. Then, the holes expanded rapidly toward higher and lower altitudes. At ∼30 min after launch, the holes extended to an altitudinal range of ∼200 km to over 700 km. The maximum depletion altitude was 425 km for the afternoon event and 283 km for the midnight event. Finally, the holes recovered slowly, with faster recovery at higher altitudes. Our work contributes to further understanding the vertical structural evolutionary mechanisms of the ionospheric holes and relevant ionospheric processes.

Abstract Image

Abstract Image

查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
三亚非相干散射雷达观测的火箭发射引发电离层空洞垂直结构演化
本文介绍了两次火箭发射过程中电离层空洞垂直结构演变的观测结果。利用新建的三亚非相干散射雷达(SYISR)和全球卫星导航系统(gps)网络的观测数据。火箭诱导的两个电离层洞在SYISR上空的垂直结构演化可分为三个阶段。首先,在发射后10-11分钟,孔洞最初出现在顶层电离层。然后,这些洞迅速向更高和更低的高度扩展。在发射后约30分钟,弹孔的高度范围从约200公里扩大到超过700公里。下午的最大耗竭高度为425公里,午夜的最大耗竭高度为283公里。最后,孔洞恢复缓慢,海拔越高恢复速度越快。本研究有助于进一步认识电离层空穴的垂直结构演化机制和相关电离层过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
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
期刊最新文献
A Statistical Survey of F2 Layer Peak Properties in the Polar Cap Ionosphere Observed by RISR-N SIFT-Based Estimation of Zonal Drift Velocity in Equatorial Plasma Bubbles Using GOLD Observations Role of Large-Scale Traveling Ionospheric Disturbances in the Positive Storm Phase Observed by the Millstone Hill Radar and GNSS TEC Measurements Role of Large-Scale Traveling Ionospheric Disturbances in the Positive Storm Phase Observed by the Millstone Hill Radar and GNSS TEC Measurements Assessment of the Generation of Traveling Ionospheric Disturbances by Solar Terminators
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1