Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015

Abstract We show the statistical characteristics of quasi-6-day wave (Q6DW) absolute amplitude in foE and foF2 during 2014–2015 by using six ionosondes at different latitudes. The results show that foE perturbations maximized at mid-latitudes during equinoxes, and the maximum amplitude of Q6DW in fo...

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Main Authors: Yi Liu, Qiong Tang, Guanyi Chen, Zhuangkai Wang, Chen Zhou
Format: Article
Language:English
Published: SpringerOpen 2020-12-01
Series:Earth, Planets and Space
Subjects:
Online Access:https://doi.org/10.1186/s40623-020-01319-7
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spelling doaj-e4bbd25ef2fa413797eac313fc6da6c32020-12-13T12:38:56ZengSpringerOpenEarth, Planets and Space1880-59812020-12-0172111310.1186/s40623-020-01319-7Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015Yi Liu0Qiong Tang1Guanyi Chen2Zhuangkai Wang3Chen Zhou4Department of Space Physics, School of Electronic Information, Wuhan UniversityDepartment of Space Physics, School of Electronic Information, Wuhan UniversityDepartment of Space Physics, School of Electronic Information, Wuhan UniversityDepartment of Space Physics, School of Electronic Information, Wuhan UniversityDepartment of Space Physics, School of Electronic Information, Wuhan UniversityAbstract We show the statistical characteristics of quasi-6-day wave (Q6DW) absolute amplitude in foE and foF2 during 2014–2015 by using six ionosondes at different latitudes. The results show that foE perturbations maximized at mid-latitudes during equinoxes, and the maximum amplitude of Q6DW in foF2 occurred near the northern crest of equatorial ionospheric anomaly (EIA). In addition, the absolute amplitude of Q6DW in foF2 increased with increasing solar activity. Our observations suggest that the dissipative Q6DW-like oscillations in the lower thermosphere may cause variations in the thermospheric neutral density via mixing effect and further result in foE disturbances in Q6DW events. Furthermore, the E region wind dynamo could also be modulated by the 6-day wave, thus leading to the disturbances in vertical plasma velocity via E × B drifts and F region electron density. Our observational investigation provides evidence of thermosphere–ionosphere coupling in the mid- and low-latitude region.https://doi.org/10.1186/s40623-020-01319-7Quasi-6-day waveAbsolute amplitude in foE and foF2Thermosphere–ionosphere coupling
collection DOAJ
language English
format Article
sources DOAJ
author Yi Liu
Qiong Tang
Guanyi Chen
Zhuangkai Wang
Chen Zhou
spellingShingle Yi Liu
Qiong Tang
Guanyi Chen
Zhuangkai Wang
Chen Zhou
Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015
Earth, Planets and Space
Quasi-6-day wave
Absolute amplitude in foE and foF2
Thermosphere–ionosphere coupling
author_facet Yi Liu
Qiong Tang
Guanyi Chen
Zhuangkai Wang
Chen Zhou
author_sort Yi Liu
title Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015
title_short Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015
title_full Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015
title_fullStr Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015
title_full_unstemmed Quasi-6-day wave effects in ionospheric E and F region during the recent solar maximum 2014–2015
title_sort quasi-6-day wave effects in ionospheric e and f region during the recent solar maximum 2014–2015
publisher SpringerOpen
series Earth, Planets and Space
issn 1880-5981
publishDate 2020-12-01
description Abstract We show the statistical characteristics of quasi-6-day wave (Q6DW) absolute amplitude in foE and foF2 during 2014–2015 by using six ionosondes at different latitudes. The results show that foE perturbations maximized at mid-latitudes during equinoxes, and the maximum amplitude of Q6DW in foF2 occurred near the northern crest of equatorial ionospheric anomaly (EIA). In addition, the absolute amplitude of Q6DW in foF2 increased with increasing solar activity. Our observations suggest that the dissipative Q6DW-like oscillations in the lower thermosphere may cause variations in the thermospheric neutral density via mixing effect and further result in foE disturbances in Q6DW events. Furthermore, the E region wind dynamo could also be modulated by the 6-day wave, thus leading to the disturbances in vertical plasma velocity via E × B drifts and F region electron density. Our observational investigation provides evidence of thermosphere–ionosphere coupling in the mid- and low-latitude region.
topic Quasi-6-day wave
Absolute amplitude in foE and foF2
Thermosphere–ionosphere coupling
url https://doi.org/10.1186/s40623-020-01319-7
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AT guanyichen quasi6daywaveeffectsinionosphericeandfregionduringtherecentsolarmaximum20142015
AT zhuangkaiwang quasi6daywaveeffectsinionosphericeandfregionduringtherecentsolarmaximum20142015
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