Articles | Volume 33, issue 7
https://doi.org/10.5194/angeo-33-913-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/angeo-33-913-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Regular paper
| 
24 Jul 2015
Regular paper |
| 24 Jul 2015
Observations of thermosphere and ionosphere changes due to the dissipative 6.5-day wave in the lower thermosphere
Q. Gan
CORRESPONDING AUTHOR
School of Electronic Information, Wuhan University, Wuhan, Hubei, China
Department of Physics and Astronomy, University of Louisville, Louisville, Kentucky, USA
Atmospheric and Planetary Sciences, Hampton University, Hampton, Virginia, USA
L. C. Chang
Institute of Space Science, National Central University, Jhongli, Taoyuan County, Taiwan
W. B. Wang
High Altitude Observatory, National Center for Atmospheric Research, Boulder, Colorado, USA
S. D. Zhang
School of Electronic Information, Wuhan University, Wuhan, Hubei, China
J. Du
Department of Physics and Astronomy, University of Louisville, Louisville, Kentucky, USA
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Cited
28 citations as recorded by crossref.
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- Study of the Quasi‐5‐Day Wave in the MLT Region by a Meteor Radar Chain Y. Gong et al. 10.1029/2018JD029355
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Latest update: 13 Dec 2024
Short summary
The 6.5-day traveling planetary wave is able to impact the ionosphere/thermosphere via a dissipation mechanism. Ionospheric TEC and thermosphere O/N2 exhibit an apparent decrease as the result of extra meridional circulation induced by 6.5-day wave dissipation. Our work suggests that the modulation of E-dynamo is not the unique pathway through which planetary waves substantially influence the IT system.
The 6.5-day traveling planetary wave is able to impact the ionosphere/thermosphere via a...
