Statistical analysis on orographic atmospheric gravity wave and sporadic E layer

被引:1
作者
Liu, Yi [1 ]
Chen, Zhou [1 ]
Fan, Zhiqiang [2 ]
Zhou, Chen [1 ]
Wang, Xiang [3 ]
Zhang, Yuqiang [1 ]
Zhou, Yufeng [2 ]
Lan, Ting [4 ]
Qing, Haiyin [5 ,6 ]
机构
[1] Wuhan Univ, Sch Elect Informat, Dept Space Phys, Wuhan 430072, Peoples R China
[2] Beijing Inst Appl Meteorol, Beijing 100101, Peoples R China
[3] Hubei Univ, Sch Artificial Intelligence, Wuhan, Peoples R China
[4] Huanggang Normal Univ, Sch Comp, Huanggang, Peoples R China
[5] Leshan Normal Univ, Sch Elect Informat & Artificial Intelligence, Leshan 614000, Peoples R China
[6] Leshan Normal Univ, Educ Dept Sichuan Prov, Key Lab Detect & Applicat Space Effect Southwest S, Leshan, Peoples R China
基金
中国国家自然科学基金;
关键词
RADIO OCCULTATION MEASUREMENTS; FIELD-ALIGNED IRREGULARITIES; IONOSPHERIC IRREGULARITIES; CONVECTION;
D O I
10.1016/j.jastp.2024.106256
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In this study, we present the statistical features of gravity wave (GW) and sporadic E layer (E S ) by using the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) data aboard the Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED) satellite and Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) radio occulation measurements during 2007 -2018. Statistical analysis of occurrences of GW and E S shows that daytime GW and E S are frequently observed on the eastern sides of the Tibetan plateau during summer, while less consistency between nighttime GW and E S occurrences was presented in our observations. The concurrence of GW and E S shows that nearly 60% E S occurred simultaneously with local strong GW occurrence. These results provide observational evidence suggesting that the effect of strong GW activities is significant in the generation of E S .
引用
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页数:8
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