Horizontal structure of convergent wind shear associated with sporadic E layers over East Asia

At present, the main detection instruments for observing sporadic E (Es) layers are ground-based radars, dense networks of ground-based global navigation satellite system (GNSS) receivers, and GNSS radio occultation, but they cannot capture the whole picture of the horizontal structure of Es layers....

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Main Authors: LiHui Qiu, Xian Lu, Tao Yu, Yosuke Yamazaki, HuiXin Liu, Yang-Yi Sun, HaoNan Wu, XiaoMin Zuo, XiangXiang Yan, Yan Yu, YiFan Qi
Format: Article
Language:English
Published: Science Press 2023-09-01
Series:Earth and Planetary Physics
Subjects:
Online Access:http://www.eppcgs.org/article/doi/10.26464/epp2023071?pageType=en
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author LiHui Qiu
Xian Lu
Tao Yu
Yosuke Yamazaki
HuiXin Liu
Yang-Yi Sun
HaoNan Wu
XiaoMin Zuo
XiangXiang Yan
Yan Yu
YiFan Qi
author_facet LiHui Qiu
Xian Lu
Tao Yu
Yosuke Yamazaki
HuiXin Liu
Yang-Yi Sun
HaoNan Wu
XiaoMin Zuo
XiangXiang Yan
Yan Yu
YiFan Qi
author_sort LiHui Qiu
collection DOAJ
description At present, the main detection instruments for observing sporadic E (Es) layers are ground-based radars, dense networks of ground-based global navigation satellite system (GNSS) receivers, and GNSS radio occultation, but they cannot capture the whole picture of the horizontal structure of Es layers. This study employs the Whole Atmosphere Community Climate Model with thermosphere and ionosphere eXtension model (WACCM-X 2.1) to derive the horizontal structure of the ion convergence region (HSICR) to explore the shapes of the large-scale Es layers over East Asia for the period from June 1 to August 31, 2008. The simulation produced the various shapes of the HSICRs elongated in the northwest−southeast, northeast−southwest, or composed of individual small patches. The close connection between Es layer critical frequency (foEs) and vertical ion convergence indicates that the HSICR is a good candidate for revealing and explaining the horizontal structure of the large-scale Es layers.
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spelling doaj.art-39542b2820d3449185a22dd712307a352023-09-05T09:56:43ZengScience PressEarth and Planetary Physics2096-39552023-09-017554855710.26464/epp2023071RA397-qiulihui-FHorizontal structure of convergent wind shear associated with sporadic E layers over East AsiaLiHui Qiu0Xian Lu1Tao Yu2Yosuke Yamazaki3HuiXin Liu4Yang-Yi Sun5HaoNan Wu6XiaoMin Zuo7XiangXiang Yan8Yan Yu9YiFan Qi10Institute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, ChinaDepartment of Physics and Astronomy, Clemson University, Clemson, SC 29631, USAInstitute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, ChinaLeibniz institute of Atmospheric Physics at the University of Rostock, 18225 Kühlungsborn, GermanyDepartment of Earth and Planetary Sciences, Kyushu University, Fukuoka 8190395, JapanInstitute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, ChinaDepartment of Physics and Astronomy, Clemson University, Clemson, SC 29631, USASchool of Mathematics and Physics, China University of Geosciences, Wuhan 430074, ChinaInstitute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, ChinaInstitute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, ChinaInstitute of Geophysics & Geomatics, China University of Geosciences, Wuhan 430074, ChinaAt present, the main detection instruments for observing sporadic E (Es) layers are ground-based radars, dense networks of ground-based global navigation satellite system (GNSS) receivers, and GNSS radio occultation, but they cannot capture the whole picture of the horizontal structure of Es layers. This study employs the Whole Atmosphere Community Climate Model with thermosphere and ionosphere eXtension model (WACCM-X 2.1) to derive the horizontal structure of the ion convergence region (HSICR) to explore the shapes of the large-scale Es layers over East Asia for the period from June 1 to August 31, 2008. The simulation produced the various shapes of the HSICRs elongated in the northwest−southeast, northeast−southwest, or composed of individual small patches. The close connection between Es layer critical frequency (foEs) and vertical ion convergence indicates that the HSICR is a good candidate for revealing and explaining the horizontal structure of the large-scale Es layers.http://www.eppcgs.org/article/doi/10.26464/epp2023071?pageType=ensporadic e layerhorizontal structurewind shearwaccm-x model
spellingShingle LiHui Qiu
Xian Lu
Tao Yu
Yosuke Yamazaki
HuiXin Liu
Yang-Yi Sun
HaoNan Wu
XiaoMin Zuo
XiangXiang Yan
Yan Yu
YiFan Qi
Horizontal structure of convergent wind shear associated with sporadic E layers over East Asia
Earth and Planetary Physics
sporadic e layer
horizontal structure
wind shear
waccm-x model
title Horizontal structure of convergent wind shear associated with sporadic E layers over East Asia
title_full Horizontal structure of convergent wind shear associated with sporadic E layers over East Asia
title_fullStr Horizontal structure of convergent wind shear associated with sporadic E layers over East Asia
title_full_unstemmed Horizontal structure of convergent wind shear associated with sporadic E layers over East Asia
title_short Horizontal structure of convergent wind shear associated with sporadic E layers over East Asia
title_sort horizontal structure of convergent wind shear associated with sporadic e layers over east asia
topic sporadic e layer
horizontal structure
wind shear
waccm-x model
url http://www.eppcgs.org/article/doi/10.26464/epp2023071?pageType=en
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