Issue |
J. Space Weather Space Clim.
Volume 14, 2024
Topical Issue - Observing, modelling and forecasting TIDs and mitigating their impact on technology
|
|
---|---|---|
Article Number | 38 | |
Number of page(s) | 12 | |
DOI | https://doi.org/10.1051/swsc/2024036 | |
Published online | 17 December 2024 |
Research Article
Medium-scale traveling ionospheric disturbances created by primary gravity waves generated by a winter storm
1
Department of Earth and Planetary Science, Kyushu University, Fukuoka, Japan
2
NASA Goddard Space Flight Center, Greenbelt, MD, USA
3
Physics Department, Catholic University of America, Washington, DC, USA
4
Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, Japan
5
High Altitude Observatory, NSF National Center for Atmospheric Research, Boulder, CO, USA
6
Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, CO, USA
* Corresponding author: kogure.masaru.055@m.kyushu-u.ac.jp
Received:
4
November
2023
Accepted:
18
November
2024
This study explores the meteorological source and vertical propagation of gravity waves (GWs) that drive daytime traveling ionospheric disturbances (TIDs), using the specified dynamics version of the SD-WACCM-X (Whole Atmosphere Community Climate Model with thermosphere-ionosphere eXtension) and the SAMI3 (Sami3 is Also a Model of the Ionosphere) simulations driven by SD-WACCM-X neutral wind and composition. A cold weather front moved over the northern-central USA (90–100°W, 35–45°N) during the daytime of 20 October 2020, with strong upward airflow. GWs with ~500–700 km horizontal wavelengths propagated southward and northward in the thermosphere over the north-central USA. Also, the perturbations were coherent from the surface to the thermosphere; therefore, the GWs were likely generated by vertical acceleration associated with the cold front over Minnesota and South Dakota. The convectively generated GWs had almost infinite vertical wavelength below ~100 km due to being evanescent. This implies that the GWs tunneled through their evanescent region in the middle atmosphere (where a squared vertical wavenumber is equal to or smaller than 0) and became freely propagating in the thermosphere and ionosphere. Medium-scale TIDs (MSTIDs) also propagated southward with the GWs, suggesting that the convectively generated GWs created MSTIDs.
Key words: Gravity wave / Medium-scale traveling ionospheric disturbance / Traveling ionospheric disturbance modeling
© M. Kogure et al., Published by EDP Sciences 2024
This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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