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Titel Relationship between strong range SF and ionospheric scintillation in low latitude ionosphere
VerfasserIn Jiankui Shi, Guojun Wang, Zheng Wang, Xiao Wang, Geliy Zherebtsov, Erina Romanova, Konst Ratovsky
Konferenz EGU General Assembly 2013
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 15 (2013)
Datensatznummer 250077692
 
Zusammenfassung
The data from the Digisondes and the ionospheric scintillation monitors located at the low latitude station Hainan (109.1°E, 19.5°N geogr., dip lat. 9°N) and Vanimo (141.3°E, 2.7°N geogr., dip lat. 11°S) are analyzed to study the ionospheric spread F (SF) and its correlation with the scintillation. According to the Digisonde observation in the low latitude ionosphere, we divide the SF as four types: range SF (R-SF), strong range SF (S-SF), frequency SF (F-SF), and mixed SF (M-SF). The S-SF is characterized by extended range spread on F layer echo traces that significantly extend beyond the local foF2 value. For the Hainan station, the results show that the maximum and minimum of the occurrence of S-SF appeared in nearly the same months as those of the GPS L-band scintillations. The variation of the S-SF occurrence was also similar to that of the scintillation. From 2003 to 2007, both the S-SF and the scintillation occurrences decreased from the high solar activity year to the low solar activity year. The correlation coefficient between the occurrences of the S-SF and the GPS L-band scintillation was as high as 0.93 suggesting associated mechanisms producing S-SF and scintillation. For the Vanimo station, the data analysis showed that the occurrence variation of the S-SF was also similar to that of the scintillation. The correlation coefficient between the two phenomena was as high as 0.88, which supports the view of the associated mechanisms to produce S-SF and scintillation. Electron density depletions extending from the bottomside to the topside ionosphere are the most likely cause explaining the high correlation.