Quasi‐biennial oscillation of the ionospheric wind dynamo. Issue 3 (7th March 2017)

• Record Type: Journal Article
• Authors: Yamazaki, Yosuke; Liu, Huixin; Sun, Yang‐Yi; Miyoshi, Yasunobu; Kosch, Michael J.; Mlynczak, Martin G.
• Is Part Of: Journal of geophysical research. Volume 122:Issue 3(2017)
• Page Start: 3553
• Page End: 3569
• Publication Date: 2017-03-07
• Subjects: QBO -- geomagnetic daily variation -- Sq current system -- interannual variability -- atmospheric tides -- GAIA model; Magnetospheric physics -- Periodicals; Space environment -- Periodicals; Cosmic physics -- Periodicals; Planets -- Atmospheres -- Periodicals; Heliosphere (Astrophysics) -- Periodicals; Geophysics -- Periodicals; 523.01
• DOI: 10.1002/2016JA023684
• Languages: English
• ISSNs: 2169-9380

Abstract

Abstract: The interannual variation of the ionospheric solar quiet ( S q ) current system is examined. A dense magnetometer network over Japan enables the accurate determination of the central position of the northern S q current loop or the S q current focus, during 1999–2015. It is found that the S q focus latitude undergoes an interannual variation of ±2° with a period of approximately 28 months, similar to the quasi‐biennial oscillation (QBO) in the tropical lower stratosphere. The QBO‐like variation of S q is particularly evident during 2005–2013. No corresponding interannual variability is found in solar extreme ultraviolet radiation. Comparisons with tidal winds, derived from a whole‐atmosphere model, reveal that the QBO‐like variation of the S q current focus is highly correlated with the amplitude variations of migrating and nonmigrating diurnal tides in the lower thermosphere. The results suggest that the stratospheric QBO can influence the ionospheric wind dynamo through the QBO modulation of tides. Key Points: A Japanese magnetometer network enables accurate determination of the central position of the ionospheric S q current loop QBO‐like variation is found in the latitudinal position of the S q current focus It correlates well with the migrating and nonmigrating tidal amplitudes in the dynamo region derived from GAIA