DocumentCode :
1920011
Title :
Investigation of the bottomside / topside contribution to the total electron content at European mid-latitudes
Author :
Zakharenkova, Irina E. ; Shagimuratov, Irk I. ; Cherniak, Iurii V. ; Krankowski, Andrzej ; Gregorczyk, Anna Krypiak-
Author_Institution :
West Dept., IZMIRAN, Kaliningrad, Russia
fYear :
2011
fDate :
13-20 Aug. 2011
Firstpage :
1
Lastpage :
1
Abstract :
Different radio sounding techniques are used to the study of the ionosphere state. In the given paper analysis of ionospheric electron density and contribution of different parts of the ionosphere to the total electron content (TEC) was carried out on the base of measurements provided by GPS transionospheric sounding, vertical ionospheric sounding and radio occultation (RO). It was considered the region of the European mid-latitudes with 2 closely located ionosonde stations - Pruhonice (50.0 N, 14.6 E) and Juliusruh (54.6 N, 13.4 E). Ionosonde data viz., ionograms, critical frequency of F2 layer (foF2) values and electron density profiles, were provided by European Digital Upper Atmosphere Server (DIAS). To obtain the bottomside ionospheric electron content (IECb) we integrate the bottomside Ne profile derived from digisonde. Topside ionosonde profile, obtained by fitting a model to the peak electron density value, was used to estimate the topside ionospheric electron content (IECt). Also the electron density profiles, derived from FormoSat-3/COSMIC RO measurements, were involved into analysis. The numerical integration was done in order to obtain COSMIC-derived IECb and IECt estimates. Therefore, for the present study the upper limit of the ionosphere has been taken to be at 750-800 km (altitude of COSMIC satellites). The total electron content values were calculated using the observations of the ground-based GPS stations located close to ionosondes. The vertical GPS TEC estimates can be split into two contributions, one part due to the bottomside ionosphere and other part due to the topside ionosphere. The topside part of TEC contains IECt and PEC (plasmaspheric electron content). So, comparison of GPS TEC, F3/C IEC and ionosonde IEC was carried out for different seasonal conditions during period of low solar activity. Special attention was focused on the differences in topside and bottomside parts contribution to TEC for night and daytime hours.
Keywords :
F-region; Global Positioning System; atmospheric structure; ionospheric measuring apparatus; radiosondes; COSMIC-derived IECb estimates; COSMIC-derived IECt estimates; DIAS; European Digital Upper Atmosphere Server; European mid-latitudes; F2 layer; FormoSat-3/COSMIC RO measurements; GPS transionospheric sounding; Juliusruh; Pruhonice; altitude 750 km to 800 km; bottomside Ne profile; bottomside contribution; bottomside ionospheric electron content; digisonde; electron density profiles; foF2 values; ionograms; ionosonde data; ionosondes; ionosphere state; ionospheric electron density; numerical integration; plasmaspheric electron content; radio occultation; radio sounding techniques; topside contribution; topside ionospheric electron content; total electron content; vertical GPS TEC estimates; vertical ionospheric sounding; Atmospheric modeling; Density measurement; Electronic mail; Europe; Global Positioning System; IEC; Ionosphere;
fLanguage :
English
Publisher :
ieee
Conference_Titel :
General Assembly and Scientific Symposium, 2011 XXXth URSI
Conference_Location :
Istanbul
Print_ISBN :
978-1-4244-5117-3
Type :
conf
DOI :
10.1109/URSIGASS.2011.6050882
Filename :
6050882
Link To Document :
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