{"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.