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赤道附近局地激发LS-TAD的事例观测
引用本文:潘建宏,蔡红涛,谷骏,周康俊,罗逸楠,高顺组.赤道附近局地激发LS-TAD的事例观测[J].地球物理学报,2022,65(3):853-861.
作者姓名:潘建宏  蔡红涛  谷骏  周康俊  罗逸楠  高顺组
作者单位:武汉大学电子信息学院,武汉430072
基金项目:科技部重大研发计划(2018YFF01013702);国家自然科学基金项目(42074185)共同资助。
摘    要:大尺度行进式大气扰动(LS-TAD)通常被认为起源于极区高纬,本文报道了一起激发于低纬赤道地区、在北半球向高纬传播的LS-TAD观测事例.2002年8月10日07:30 UT,CHAMP卫星在30°W磁赤道附近观测到显著的大气密度增强,在随后的2个连续轨道上,该密度增强依次出现在北半球更高纬度上,表现出明显的极向位移,...

关 键 词:赤道区域  离子垂直漂移  LS-TAD  LS-TIDI

A case study of large-scale travelling atmospheric disturbances driven by equatorial local source
PAN JianHong,CAI HongTao,GU Jun,ZHOU KangJun,LUO YiNan,GAO ShunZu.A case study of large-scale travelling atmospheric disturbances driven by equatorial local source[J].Chinese Journal of Geophysics,2022,65(3):853-861.
Authors:PAN JianHong  CAI HongTao  GU Jun  ZHOU KangJun  LUO YiNan  GAO ShunZu
Institution:(Electronic Information School,Wuhan University,Wuhan 430072,China)
Abstract:Large-Scale Travelling Atmospheric Disturbance(LS-TAD)is generally believed to originate from the high-latitude auroral areas and then propagate equatorward.In this paper,we report a case of LS-TAD which was stimulated in low-latitude equatorial regions and propagated toward higher latitudes in the Northern hemisphere.CHAMP spacecraft encountered a remarkable neutral density enhancement at equatorial region during its flight over South America about 07∶30 UT on 10th Aug.2002.The density enhancements were detected during the following 3 flyovers at higher latitude in the Northern Hemisphere.Remarkable latitudinal displacement of the density enhancement suggests presence of a LS-TAD.Meanwhile,evidences of Large-Scale Travelling Ionospheric Disturbance(LS-TID),which is generally accompanied by LS-TAD,was recorded by two ground-based GNSS chains.We find no signatures of travelling disturbances in Southern Hemisphere,which are related to the aforementioned LS-TAD/TID.We suggest that the observed LS-TAD was likely to originate from equatorial region,driven by an abrupt increasement of ion vertical drift.
Keywords:Equatorial regions  Ion vertical drift  LS-TAD LS-TID
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