Comparison of the tidal signatures in sporadic E and vertical ion convergence rate, using FORMOSAT-3/COSMIC radio occultation observations and GAIA model

Comparison of the tidal signatures in sporadic E and vertical ion convergence rate, using FORMOSAT-3/COSMIC radio occultation observations and GAIA model

Abstract Sporadic E or Es is a transient phenomenon where thin layers of enhanced electron density appear in the ionospheric E region (90–120 km altitude). The neutral wind shear caused by atmospheric tides can lead ions to converge vertically at E-region heights and form the Es layer. This research...

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Bibliographic Details
Main Authors: Sahar Sobhkhiz-Miandehi, Yosuke Yamazaki, Christina Arras, Yasunobu Miyoshi, Hiroyuki Shinagawa
Format: Article
Language:English
Published: SpringerOpen 2022-06-01
Series:Earth, Planets and Space
Subjects:
Sporadic E
Es
Wind shear
Solar tide
Lunar tide
GAIA
Online Access:https://doi.org/10.1186/s40623-022-01637-y

Internet

https://doi.org/10.1186/s40623-022-01637-y

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