Simultaneous and common-volume three-lidar observations of sporadic metal layers in the mesopause region

被引:15
|
作者
Yi, Fan [1 ,2 ,3 ]
Zhang, Shaodong [1 ,2 ,3 ]
Yu, Changming [1 ,2 ,3 ]
Zhang, Yunpeng [1 ,2 ,3 ]
He, Yujin [1 ,2 ,3 ]
Liu, Fuchao [1 ,2 ,3 ]
Huang, Kaiming [1 ,2 ,3 ]
Huang, Chunming [1 ,2 ,3 ]
Tan, Ying [1 ,2 ,3 ]
机构
[1] Wuhan Univ, Sch Elect Informat, Wuhan 430072, Peoples R China
[2] Minist Educ, Key Lab Geospace Environm & Geodesy, Wuhan 430072, Peoples R China
[3] State Observ Atmospher Remote Sensing, Wuhan 430072, Peoples R China
基金
中国国家自然科学基金;
关键词
Sporadic metal layer; Multi-metal mixture; Mesopause region; Three-lidar observation; NA METEOR TRAILS; LIDAR OBSERVATIONS; SODIUM LAYERS; WUHAN; 30.5-DEGREES-N; MESOSPHERIC NA; CA+ LAYERS; FE LAYERS; CHEMISTRY; ARECIBO; IRON;
D O I
10.1016/j.jastp.2013.05.013
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
We report on the first simultaneous three-lidar observations of sporadic metal layers in the mesopause region. The case studies indicate that the sporadic layering events can be observed generally in three neutral metal atom species (Na, Fe and Ca) or two neutral atom and one ion species (Na, Fe and Ca+). The density enhancements of all the sporadic metal atom and ion species occurred in overlapping altitude range and moved following almost the same track, indicating that the sporadic metal layers are usually a mixture of multiple metal atom and ion species, meanwhile suggesting that all these metal species in a mixture are product of the same or similar source processes. Some strong multi-metal sporadic layering events were found to manifest a regular altitude relation that the Na-s is highest, the Fe-s is a few to tens of hundreds of meters lower than the Nas, while the Ca-s is a few hundred meters lower than the Fes, and the Ca-s(+) is lowest. This altitude sequence coincides well with the boiling-point dependent differential ablation in the thermal ablation theory. For those weak multi-metal sporadic events, the altitude relation becomes complicated. Profiles from two short sequences of a single night show that the formation/variation of the Ca-s(+) layer features appeared to follow the related Na-s and Fe-s layer features with a delayed period of similar to 5 min. At altitudes above 105 km, weak single-species Ca-s(+) layers were occasionally observed. This appears to reflect a feature of the sputtering ablation. For the explanation of our observations the formation mechanism issues of sporadic metal layers are discussed in detail. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:172 / 184
页数:13
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