Postmidnight equatorial plasma irregularities on the June solstice during low solar activity – a case study
Autor: | Chi Wang, F. Becker-Guedes, Jonathan J. Makela, Narayan P. Chapagain, Zhengkuan Liu, Inez S. Batista, Emilia Correia, Jiankui Shi, M. A. Abdu, Claudia Maria Nicoli Candido, N. Balan |
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Jazyk: | angličtina |
Rok vydání: | 2019 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Magnetic dip 01 natural sciences Wind speed 0103 physical sciences Earth and Planetary Sciences (miscellaneous) Solstice Field aligned irregularities lcsh:Science 010303 astronomy & astrophysics 0105 earth and related environmental sciences Advection lcsh:QC801-809 Airglow Geology Astronomy and Astrophysics Plasma Geodesy lcsh:QC1-999 Interferometry lcsh:Geophysics. Cosmic physics TheoryofComputation_MATHEMATICALLOGICANDFORMALLANGUAGES Space and Planetary Science lcsh:Q lcsh:Physics |
Zdroj: | Annales Geophysicae, Vol 37, Pp 657-672 (2019) |
ISSN: | 1432-0576 0992-7689 |
Popis: | We present a case study of unusual spread-F structures observed by ionosondes at two equatorial and low-latitude Brazilian stations – São Luís (SL: 44.2∘ W, 2.33∘ S; dip angle: −6.9∘) and Fortaleza (FZ: 38.45∘ W, 3.9∘ S; dip angle: −16∘). The irregularity structures observed from midnight to postmidnight hours of moderate solar activity (F10.7 < 97 sfu, where 1 sfu = 10−22 W m−2 s−1) have characteristics different from typical post-sunset equatorial spread F. The spread-F traces first appeared at or above the F-layer peak and gradually became well-formed mixed spread F. They also appeared as plasma depletions in the 630.0 nm airglow emissions made by a wide-angle imager located at the nearby low-latitude station Cajazeiras (CZ: 38.56∘ W, 6.87∘ S; dip angle: −21.4∘). The irregularities appeared first over FZ and later over SL, giving evidence of an unusual westward propagation or a horizontal plasma advection. The drift-mode operation available in one of the ionosondes (a digital portable sounder, DPS-4) has enabled us to analyze the horizontal drift velocities and directions of the irregularity movement. We also analyzed the neutral wind velocity measured by a Fabry–Pérot interferometer (FPI) installed at CZ and discuss its possible role in the development of the irregularities. |
Databáze: | OpenAIRE |
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