Effects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic model
In addition to being driven by tidal winds, the sporadic E (Es) layers are modulated by gravity waves (GWs), although the effects are not yet comprehensively understood. In this article, we discuss the effects of mesoscale GWs on the Es layers determined by using a newly developed model, MISE-1D (on...
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Science Press
2025-01-01
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Online Access: | http://www.eppcgs.org/article/doi/10.26464/epp2024038?pageType=en |
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author | Xu Zhou ZeZhong Li XinAn Yue LiBo Liu |
author_facet | Xu Zhou ZeZhong Li XinAn Yue LiBo Liu |
author_sort | Xu Zhou |
collection | DOAJ |
description | In addition to being driven by tidal winds, the sporadic E (Es) layers are modulated by gravity waves (GWs), although the effects are not yet comprehensively understood. In this article, we discuss the effects of mesoscale GWs on the Es layers determined by using a newly developed model, MISE-1D (one-dimensional Model of Ionospheric Sporadic E), with low numerical dissipation and high resolution. Driven by the wind fields resolved by the high-resolution version of the Whole Atmosphere Community Climate Model with thermosphere and ionosphere extension (WACCM-X), the MISE-1D simulation revealed that GWs significantly influence the evolution of the Es layer above 100 km but have a very limited effect at lower altitudes. The effects of GWs are diverse and complex, generally including the generation of fluctuating wavelike structures on the Es layer with frequencies similar to those of the GWs. The mesoscale GWs can also cause increases in the density of Es layers, or they can disperse or diffuse the Es layers and increase their thickness. In addition, the presence of GWs is a key factor in sustaining the Es layers in some cases. |
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institution | Kabale University |
issn | 2096-3955 |
language | English |
publishDate | 2025-01-01 |
publisher | Science Press |
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series | Earth and Planetary Physics |
spelling | doaj-art-2e0e6ca0d3dc45e3910aa4cfeac0b9702025-01-06T07:40:39ZengScience PressEarth and Planetary Physics2096-39552025-01-01911910.26464/epp2024038S20487-zhouxu-FEffects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic modelXu Zhou0ZeZhong Li1XinAn Yue2LiBo Liu3Key Laboratory of Earth and Planetary Physics/Heilongjiang Mohe National Geophysical Observatory/Beijing National Observatory of Space Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences (CAS), Beijing 100029, ChinaCAS Center for Excellence in Comparative Planetology/CAS Key Laboratory of Geospace Environment/Mengcheng National Geophysical Observatory, University of Science and Technology of China, Hefei 230026, ChinaKey Laboratory of Earth and Planetary Physics/Heilongjiang Mohe National Geophysical Observatory/Beijing National Observatory of Space Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences (CAS), Beijing 100029, ChinaKey Laboratory of Earth and Planetary Physics/Heilongjiang Mohe National Geophysical Observatory/Beijing National Observatory of Space Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences (CAS), Beijing 100029, ChinaIn addition to being driven by tidal winds, the sporadic E (Es) layers are modulated by gravity waves (GWs), although the effects are not yet comprehensively understood. In this article, we discuss the effects of mesoscale GWs on the Es layers determined by using a newly developed model, MISE-1D (one-dimensional Model of Ionospheric Sporadic E), with low numerical dissipation and high resolution. Driven by the wind fields resolved by the high-resolution version of the Whole Atmosphere Community Climate Model with thermosphere and ionosphere extension (WACCM-X), the MISE-1D simulation revealed that GWs significantly influence the evolution of the Es layer above 100 km but have a very limited effect at lower altitudes. The effects of GWs are diverse and complex, generally including the generation of fluctuating wavelike structures on the Es layer with frequencies similar to those of the GWs. The mesoscale GWs can also cause increases in the density of Es layers, or they can disperse or diffuse the Es layers and increase their thickness. In addition, the presence of GWs is a key factor in sustaining the Es layers in some cases.http://www.eppcgs.org/article/doi/10.26464/epp2024038?pageType=ensporadic eion tidal layergravity wavesnumerical simulation |
spellingShingle | Xu Zhou ZeZhong Li XinAn Yue LiBo Liu Effects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic model Earth and Planetary Physics sporadic e ion tidal layer gravity waves numerical simulation |
title | Effects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic model |
title_full | Effects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic model |
title_fullStr | Effects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic model |
title_full_unstemmed | Effects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic model |
title_short | Effects of mesoscale gravity waves on sporadic E simulated by a one-dimensional dynamic model |
title_sort | effects of mesoscale gravity waves on sporadic e simulated by a one dimensional dynamic model |
topic | sporadic e ion tidal layer gravity waves numerical simulation |
url | http://www.eppcgs.org/article/doi/10.26464/epp2024038?pageType=en |
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