Form of presentation | Articles in international journals and collections |
Year of publication | 2017 |
Язык | английский |
|
Akchurin Adel Dzhavidovich, author
Sherstyukov Oleg Nikolaevich, author
Sherstyukov Ruslan Olegovich, author
|
Bibliographic description in the original language |
R.O. Sherstyukov, A.D. Akchurin , O.N. Sherstyukov Collocated ionosonde and dense GPS/GLONASS network measurements of midlatitude MSTIDs // Advances in Space Research, 2017DOI:10.1016/j.asr.2017.11.026 http://www.sciencedirect.com/science/article/pii/S0273117717308372 |
Annotation |
To analyze midlatitude medium-scale travelling ionospheric disturbances (MSTIDs) over Kazan (55.5?N, 49?E), Russia, the sufficiently dense network of GNSS receivers (more than 150 ground-based stations) were used. For the first time, daytime MSTIDs in the form of their main signature (band structure) on high-resolution two-dimensional maps of the total electron content perturbation (TEC maps) are compared with ionosonde data with a high temporal resolution. For a pair of events, a relationship between southwestward TEC perturbations and evolution of F2 layer traces was established. So F2 peak frequency varied in antiphase to TEC perturbations. The ionograms show that during the movement of plasma depletion band (overhead ionosonde) the F2 peak frequency is the highest, and vice versa, for the plasma enhancement band, the F2 peak frequency is the lowest. One possible explanation may be a greater inclination of the radio beam from the vertical during the placement of a plasma enhancement |
Keywords |
electron content perturbation, ionosonde, travelling ionospheric disturbances |
The name of the journal |
Advances in Space Research
|
URL |
http://www.sciencedirect.com/science/article/pii/S0273117717308372 |
Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=169350&p_lang=2 |
Full metadata record |
Field DC |
Value |
Language |
dc.contributor.author |
Akchurin Adel Dzhavidovich |
ru_RU |
dc.contributor.author |
Sherstyukov Oleg Nikolaevich |
ru_RU |
dc.contributor.author |
Sherstyukov Ruslan Olegovich |
ru_RU |
dc.date.accessioned |
2017-01-01T00:00:00Z |
ru_RU |
dc.date.available |
2017-01-01T00:00:00Z |
ru_RU |
dc.date.issued |
2017 |
ru_RU |
dc.identifier.citation |
R.O. Sherstyukov, A.D. Akchurin , O.N. Sherstyukov Collocated ionosonde and dense GPS/GLONASS network measurements of midlatitude MSTIDs // Advances in Space Research, 2017DOI:10.1016/j.asr.2017.11.026 http://www.sciencedirect.com/science/article/pii/S0273117717308372 |
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/eng/?p_id=169350&p_lang=2 |
ru_RU |
dc.description.abstract |
Advances in Space Research |
ru_RU |
dc.description.abstract |
To analyze midlatitude medium-scale travelling ionospheric disturbances (MSTIDs) over Kazan (55.5?N, 49?E), Russia, the sufficiently dense network of GNSS receivers (more than 150 ground-based stations) were used. For the first time, daytime MSTIDs in the form of their main signature (band structure) on high-resolution two-dimensional maps of the total electron content perturbation (TEC maps) are compared with ionosonde data with a high temporal resolution. For a pair of events, a relationship between southwestward TEC perturbations and evolution of F2 layer traces was established. So F2 peak frequency varied in antiphase to TEC perturbations. The ionograms show that during the movement of plasma depletion band (overhead ionosonde) the F2 peak frequency is the highest, and vice versa, for the plasma enhancement band, the F2 peak frequency is the lowest. One possible explanation may be a greater inclination of the radio beam from the vertical during the placement of a plasma enhancement |
ru_RU |
dc.language.iso |
ru |
ru_RU |
dc.subject |
electron content perturbation |
ru_RU |
dc.subject |
ionosonde |
ru_RU |
dc.subject |
travelling ionospheric disturbances |
ru_RU |
dc.title |
Collocated ionosonde and dense GPS/GLONASS network measurements of midlatitude MSTIDs |
ru_RU |
dc.type |
Articles in international journals and collections |
ru_RU |
|