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    請使用永久網址來引用或連結此文件: https://ir.lib.ncu.edu.tw/handle/987654321/102321


    題名: Strong ionospheric field-aligned currents for radial interplanetary magnetic fields
    作者: 許志浤;Wang, Hui;Lühr, Hermann;Shue, Jih-Hong;Frey, Harald. U.;Kervalishvili, Guram;Huang, Tao;Cao, Xue;Pi, Gilbert;Ridley, Aaron J.
    貢獻者: 地球科學學院太空科學與工程學系
    關鍵詞: air upwelling;field-aligned currents;Flow channels;Flow pattern;Geophysics;Ionosphere;Magnetic fields;Polarity;radial interplanetary magnetic field
    日期: 2014-01-01
    上傳時間: 2026-04-23 11:06:16 (UTC+8)
    出版者: Wiley-Blackwell;Washington: Blackwell Publishing Ltd
    摘要: 摘要: AbstractThe present work has investigated the configuration of field‐aligned currents (FACs) during a long period of radial interplanetary magnetic field (IMF) on 19 May 2002 by using high‐resolution and precise vector magnetic field measurements of CHAMP satellite. During the interest period IMF By and Bz are weakly positive and Bx keeps pointing to the Earth for almost 10 h. The geomagnetic indices Dst is about −40 nT and AE about 100 nT on average. The cross polar cap potential calculated from Assimilative Mapping of Ionospheric Electrodynamics and derived from DMSP observations have average values of 10–20 kV. Obvious hemispheric differences are shown in the configurations of FACs on the dayside and nightside. At the south pole FACs diminish in intensity to magnitudes of about 0.1 μA/m2, the plasma convection maintains two‐cell flow pattern, and the thermospheric density is quite low. However, there are obvious activities in the northern cusp region. One pair of FACs with a downward leg toward the pole and upward leg on the equatorward side emerge in the northern cusp region, exhibiting opposite polarity to FACs typical for duskward IMF orientation. An obvious sunward plasma flow channel persists during the whole period. These ionospheric features might be manifestations of an efficient magnetic reconnection process occurring in the northern magnetospheric flanks at high latitude. The enhanced ionospheric current systems might deposit large amount of Joule heating into the thermosphere. The air densities in the cusp region get enhanced and subsequently propagate equatorward on the dayside. Although geomagnetic indices during the radial IMF indicate low‐level activity, the present study demonstrates that there are prevailing energy inputs from the magnetosphere to both the ionosphere and thermosphere in the northern polar cusp region.
    其他題名: J. Geophys. Res. Space Physics
    出版者: Washington: Blackwell Publishing Ltd
    出版日期: 2014-05
    出處: Journal of Geophysical Research: Space Physics, 2014-05, Vol.119 (5), p.3979-3995
    資源來源: Wiley Online Library Journals AutoHoldings
    版權: 2014. American Geophysical Union. All Rights Reserved.
    識別號: ISSN: 2169-9380
    識別號: ISSN: 2169-9402
    識別號: EISSN: 2169-9402
    識別號: DOI: 10.1002/2014JA019951
    顯示於類別:[太空科學與工程學系] 期刊論文

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