H. Takahashi, C. Figueiredo, P. Essien, C. M. Wrasse, D. Barros, P. K. Nyassor, I. Paulino, F. Egito, Geângelo de Matos Rosa, Antonio Hélder Rodrigues Sampaio
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引用次数: 2
Abstract
Abstract. We observed a gravity wave (GW) signature in the OH
emission layer in the upper mesosphere, and 4 h later, a medium-scale
travelling ionospheric disturbance (MSTID) in the OI 630 nm emission layer.
Spectral analysis of the two waves showed that both have almost the same
wave characteristics: wavelength, period, phase speed and propagation
direction, respectively, 200 km, 60 min, 50 m s−1, toward the southeast. From
the gravity wave ray-tracing simulation for the mesospheric gravity wave, we
found that the wave came from a tropospheric deep convection spot and
propagated up to the 140 km altitude. Regarding the same wave
characteristics between mesospheric GW and ionospheric MSTID, the two
possible cases are investigated: a direct influence of the GW oscillation in
the OI 630 nm emission height and the generation of a secondary wave during
the GW breaking process. This is the first time to report an observational
event of gravity wave propagation from the troposphere, mesosphere to
thermosphere–ionosphere in the South American region.
期刊介绍:
Annales Geophysicae (ANGEO) is a not-for-profit international multi- and inter-disciplinary scientific open-access journal in the field of solar–terrestrial and planetary sciences. ANGEO publishes original articles and short communications (letters) on research of the Sun–Earth system, including the science of space weather, solar–terrestrial plasma physics, the Earth''s ionosphere and atmosphere, the magnetosphere, and the study of planets and planetary systems, the interaction between the different spheres of a planet, and the interaction across the planetary system. Topics range from space weathering, planetary magnetic field, and planetary interior and surface dynamics to the formation and evolution of planetary systems.