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Ionospheric vertical plasma drift perturbations due to the quasi 2day wave

机译:Ionospheric vertical plasma drift perturbations due to the quasi 2day wave

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摘要

abstract_textpThe thermosphere-ionosphere-mesosphere-electrodynamics-general circulation model is utilized to study the vertical E x B drift perturbations due to the westward quasi 2 day wave with zonal wave numbers 2 and 3 (W2 and W3). The simulations show that both wind components contribute directly and significantly to the vertical drift, which is not merely confined to low latitudes. The vertical drifts at the equator induced by the total wind perturbations of W2 are comparable with that at middle latitudes, while the vertical drifts from W3 are much stronger at middle latitudes than at the equator. The ion drift perturbations induced by the zonal and meridional wind perturbations of W2 are nearly in-phase with each other, whereas the phase discrepancies of the ion drift induced by the individual wind component of W3 are much larger. This is because the wind perturbations of W2 and W3 have different latitudinal structures and phases, which result in different ionospheric responses through wind dynamo./p/abstract_text

著录项

  • 来源
    《Journal of geophysical research》 |2015年第5期|3941-3948|共8页
  • 作者单位

    Univ Sci & Technol China, CAS Key Lab Geospace Environm, Dept Geophys & Planetary Sci, Hefei 230026, Peoples R China;

    Chinese Acad Sci, Sate Key Lab Space Weather, Beijing, Peoples R China;

    Univ Sci & Technol China, Mengcheng Natl Geophys Observ, Sch Earth & Space Sci, Hefei 230026, Peoples R ChinaChinese Acad Sci, Key Lab Earth & Planetary Phys, Inst Geol & Geophys, Beijing, Peoples R ChinaNatl Ctr Atmospher Res, High Altitude Observ, Boulder, CO 80307 USA;

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  • 原文格式 PDF
  • 正文语种 英语
  • 中图分类
  • 关键词

    2-DAY OSCILLATION; QUASI-2-DAY WAVE; ATMOSPHERE; MIDDLE;

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