Electron density profiles deduced from GPS TEC, O+-H+transition height and ionosonde data

N. Jakowski, S. Stankov, I. Kutiev
{"title":"Electron density profiles deduced from GPS TEC, O+-H+transition height and ionosonde data","authors":"N. Jakowski, S. Stankov, I. Kutiev","doi":"10.1556/AGEOD.37.2002.2-3.6","DOIUrl":null,"url":null,"abstract":"A new formula of the electron density profiles above the peak height is introduced. The formula is based on the Epstein layer and depends on the O and H scale heights and the OH transition level. Both scale heights have a ratio 1:16 reduced by a factor representing the change from magnetic field line direction to vertical direction. The bottom-side part of TEC (calculated by using foF2, M3000F2 and foE measurements) is subtracted from the GPSderived TEC at the same location. The topside TEC, together with the empirically obtained O-H transition level, are then used to deduce the unknown scale heights. The method is demonstrated on actual data covering low and high solar activity conditions.","PeriodicalId":50900,"journal":{"name":"Acta Geodaetica et Geophysica Hungarica","volume":"37 1","pages":"171-181"},"PeriodicalIF":0.0000,"publicationDate":"2002-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"12","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Geodaetica et Geophysica Hungarica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1556/AGEOD.37.2002.2-3.6","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 12

Abstract

A new formula of the electron density profiles above the peak height is introduced. The formula is based on the Epstein layer and depends on the O and H scale heights and the OH transition level. Both scale heights have a ratio 1:16 reduced by a factor representing the change from magnetic field line direction to vertical direction. The bottom-side part of TEC (calculated by using foF2, M3000F2 and foE measurements) is subtracted from the GPSderived TEC at the same location. The topside TEC, together with the empirically obtained O-H transition level, are then used to deduce the unknown scale heights. The method is demonstrated on actual data covering low and high solar activity conditions.
从GPS TEC、O+-H+跃迁高度和离子探空仪数据推导出的电子密度剖面
提出了一个新的峰高以上电子密度分布公式。该公式基于爱泼斯坦层,取决于O和H标度高度以及OH跃迁能级。两个标尺高度的比例都是1:16,减少的因子表示从磁力线方向到垂直方向的变化。从同一位置的gps导出的TEC中减去TEC的底部部分(通过使用foF2, M3000F2和foE测量计算)。然后使用上部TEC和经验获得的O-H过渡水平来推断未知的尺度高度。该方法在太阳活动高低两种情况下的实测数据上得到了验证。
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 求助全文
来源期刊
Acta Geodaetica et Geophysica Hungarica
Acta Geodaetica et Geophysica Hungarica 地学-地球化学与地球物理
自引率
0.00%
发文量
0
审稿时长
3 months
×
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
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
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 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信