Equatorial rising structure in nighttime upper E-region: A manifestation of electrodynamical coupling of spread F

Journal of Atmospheric and Solar-Terrestrial Physics

Volumn 64, Issue 12-14, 2002, Pages 1505-1510

  Kherani, E A ^a   Raghavarao, R ^b   Sekar, R ^a  

^a PHYSICAL RESEARCH LABORATORY   (India)

^b Nitya Laboratories Ltd   (India)

Author keywords

Equatorial ionosphere; Equatorial spread F; Plasma irregularities

Indexed keywords

ATMOSPHERIC STRUCTURE; E REGION; F REGION; IONOSPHERE; PLASMA;

EID: 0036672856     PISSN: 13646826     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1364-6826(02)00087-1     Document Type: Article

References (17)

1. Scintillations, plasma drifts, and neutral winds in the equatorial ionosphere after sunset
2. Kilometric irregularities in the E and F regions of the daytime equatorial ionosphere observed by a high resolution HF radar
3. High resolution radar observations of daytime kilometer scale wave structure in the equatorial electrojet
4. The effect of vertical drift on the equatorial F region stability
5. Seeding and layering of equatorial spread-F by gravity waves
6. Gravity wave interaction of equatorial spread-F: A case study
7. High-resolution radar measurements of turbulent structure in the low latitude E-region
8. Nonlinear numerical simulation of equatorial spread-F effects of winds and electric fields
9. Neutral temperature anomoly in the equatorial thermosphere-a source of vertical winds
10. Equatorial spread-F (ESF) and vertical winds
11. Effects of vertical winds and electric fields in the nonlinear evolution of equatorial spread-F
12. Equatorial plasma bubble evolution and its role in the generation of irregularities in the lower F-region
13. Interaction of two long wavelength modes in the nonlinear numerical simulation model of equatorial spread F
14. High-resolution radar measurements of turbulent structures in the equatorial electrojet
15. Equatorial quasiperiodic echoes from field-aligned irregularities observed over Jicamarca
16. Radar observation of F-region equatorial irregularities
17. Nonlinear equatorial spread-F: Spatially large bubbles resulting from large horizontal scale initial perturbations