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Interaction Between a Southwestward Propagating MSTID and a Poleward Moving WSA‐Like Plasma Patch on a Magnetically Quiet Night at Midlatitude China Region
Author(s) -
Sun Longchang,
Xu Jiyao,
Zhu Yajun,
Yuan Wei,
Chen Zhiqing,
Hao Yongqiang,
Hu Lianhuan,
Zhang Donghe,
Guo Bing,
Zhao Xiukuan
Publication year - 2020
Publication title -
journal of geophysical research: space physics
Language(s) - English
Resource type - Journals
eISSN - 2169-9402
pISSN - 2169-9380
DOI - 10.1029/2020ja028085
Subject(s) - middle latitudes , ionosphere , airglow , atmospheric sciences , plasma , f region , geology , sporadic e propagation , anomaly (physics) , climatology , geophysics , physics , quantum mechanics , condensed matter physics
In this paper, we first investigate the effects of a postevening Weddell Sea Anomaly (WSA)‐like plasma patch on a southwestward propagating medium‐scale traveling ionospheric disturbance (MSTID) over Xinglong, China (40.4°N, 117.6°E; Mlat. ~30.4°N). We found that some of this kind of WSA‐like plasma patches moved northward from the equatorial ionization anomaly (EIA) regions to midlatitudes, as they traveled westward into China. During 2012–2016, these plasma patches frequently occurred during the period of May–August with a monthly occurrence rate of over 20%, causing nighttime plasma density enhancements (NPDEs) in midlatitudes of China. Over 50% of these structures were accompanied by concurrent MSTID and Es . We propose that an intense polarization electric field (PEF) associated with an MSTID/ Es from the more northern regions of EIA could frequently drive these plasma patches poleward. On the night of 27 June 2014 ( Kp < 2 − ), either an MSTID and an intense Es layer (the maximum foEs >12 MHz) occurred at the onset of the poleward motion of a WSA‐like plasma patch, lending credence to this possibility. The observed plasma patch was pushed poleward to interact with the observed MSTID, causing some poleward extending C‐shaped airglow depletions/enhancements of the MSTID in a transition region where the ionosphere changed from a collapse region to an uplifted one. We attributed those poleward extending airglow depletions to the interaction between the MSTID and the plasma patch because of the secondary gradient drift instability and those of airglow enhancements to the redistribution of plasma.