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....
Main Authors: | , , , , , , , , , , |
---|---|
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 |
_version_ | 1797692520762703872 |
---|---|
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. |
first_indexed | 2024-03-12T02:28:48Z |
format | Article |
id | doaj.art-39542b2820d3449185a22dd712307a35 |
institution | Directory Open Access Journal |
issn | 2096-3955 |
language | English |
last_indexed | 2024-03-12T02:28:48Z |
publishDate | 2023-09-01 |
publisher | Science Press |
record_format | Article |
series | Earth and Planetary Physics |
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 |
work_keys_str_mv | AT lihuiqiu horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT xianlu horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT taoyu horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT yosukeyamazaki horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT huixinliu horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT yangyisun horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT haonanwu horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT xiaominzuo horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT xiangxiangyan horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT yanyu horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia AT yifanqi horizontalstructureofconvergentwindshearassociatedwithsporadicelayersovereastasia |