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...

Full description

Saved in:
Bibliographic Details
Main Authors: Xu Zhou, ZeZhong Li, XinAn Yue, LiBo Liu
Format: Article
Language:English
Published: Science Press 2025-01-01
Series:Earth and Planetary Physics
Subjects:
Online Access:http://www.eppcgs.org/article/doi/10.26464/epp2024038?pageType=en
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1841558628517019648
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.
format Article
id doaj-art-2e0e6ca0d3dc45e3910aa4cfeac0b970
institution Kabale University
issn 2096-3955
language English
publishDate 2025-01-01
publisher Science Press
record_format Article
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
work_keys_str_mv AT xuzhou effectsofmesoscalegravitywavesonsporadicesimulatedbyaonedimensionaldynamicmodel
AT zezhongli effectsofmesoscalegravitywavesonsporadicesimulatedbyaonedimensionaldynamicmodel
AT xinanyue effectsofmesoscalegravitywavesonsporadicesimulatedbyaonedimensionaldynamicmodel
AT liboliu effectsofmesoscalegravitywavesonsporadicesimulatedbyaonedimensionaldynamicmodel