On the source of the polar wind in the polar topside ionosphere: First results from the EISCAT Svalbard radar
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- Y. Ogawa
- National Institute of Polar Research Tachikawa Japan
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- I. Häggström
- EISCAT Scientific Association Kiruna Sweden
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- S. C. Buchert
- Swedish Institute of Space Phyics Uppsala Sweden
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- K. Oksavik
- Arctic Geophyisic UNIS Longyearbyen Norway
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- S. Nozawa
- Solar‐Terrestrial Environment Laboratory Nagoya University Nagoya Japan
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- M. Hirahara
- Department of Physics Rikkyo University Tokyo Japan
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- A. P. van Eyken
- EISCAT Scientific Association Longyearbyen Norway
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- T. Aso
- National Institute of Polar Research Tokyo Japan
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- R. Fujii
- Solar‐Terrestrial Environment Laboratory Nagoya University Nagoya Japan
書誌事項
- 公開日
- 2009-12
- 資源種別
- journal article
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2009gl041501
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
<jats:p>We present quantitative radar observations of both hydrogen ion (H<jats:sup>+</jats:sup>) and oxygen ion (O<jats:sup>+</jats:sup>) upflow in the topside polar ionosphere using measurements that were recently carried out with the EISCAT Svalbard Radar and the Reimei satellite. H<jats:sup>+</jats:sup> upflow was clearly observed equatorward of the cusp above 500 km altitude. Within the cusp the H<jats:sup>+</jats:sup> density was very low, and the upflow was dominated by O<jats:sup>+</jats:sup> ions, but on closed field lines the H<jats:sup>+</jats:sup> became the larger contributor to the upward flux above about 550 km. The total flux seemed to be conserved, and so below 550 km altitude O<jats:sup>+</jats:sup> (with a small upward velocity of ∼50 m s<jats:sup>−1</jats:sup>) appeared to determine the upward flux which was then maintained by H<jats:sup>+</jats:sup> in the topside ionosphere. We also found that the H<jats:sup>+</jats:sup> density in the topside polar ionosphere was several times higher than current predictions of ionospheric models like IRI2001.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 36 (24), L24103-, 2009-12
American Geophysical Union (AGU)
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詳細情報 詳細情報について
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- CRID
- 1360004233285672832
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- ISSN
- 19448007
- 00948276
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- 資料種別
- journal article
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- データソース種別
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- Crossref
- KAKEN
- OpenAIRE

