Equatorward moving auroral signatures of a flow burst observed prior to auroral onset
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- L. Kepko
- Space Science Center University of New Hampshire Durham New Hampshire USA
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- E. Spanswick
- Department of Physics and Astronomy University of Calgary Calgary, Alberta Canada
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- V. Angelopoulos
- Institute of Geophysics and Planetary Physics University of California Los Angeles California USA
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- E. Donovan
- Department of Physics and Astronomy University of Calgary Calgary, Alberta Canada
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- J. McFadden
- Space Sciences Laboratory University of California at Berkeley California USA
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- K.‐H. Glassmeier
- Institute of Geophysics and Extraterrestrial Physics Technical University of Braunschweig Braunschweig Germany
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- J. Raeder
- Space Science Center University of New Hampshire Durham New Hampshire USA
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- H. J. Singer
- Space Weather Prediction Center NOAA Boulder Colorado USA
書誌事項
- 公開日
- 2009-12
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2009gl041476
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
<jats:p>We present observations of a substorm that occurred on February 25, 2008. Auroral onset was observed with a multi‐spectral (<jats:italic>λ</jats:italic> = 427.8, 557.7 and 630.0 nm) and white light all sky imager at Gillam, Canada. An equatorward moving diffuse auroral patch was observed in the <jats:italic>λ</jats:italic> = 630.0 nm images at least six minutes prior to auroral onset. This form emerged from the background noise poleward of the eventual onset arc and intensified as it moved equatorward. Auroral expansion onset occurred when this form reached the onset arc location. Flows were detected by THEMIS probes P3 (TH‐D) and P4 (TH‐E) near <jats:italic>X</jats:italic> ∼ −11 <jats:italic>R</jats:italic><jats:sub><jats:italic>E</jats:italic></jats:sub> nearly 90 seconds prior to auroral expansion. A small discrete arc was observed in the <jats:italic>λ</jats:italic> = 557.7 nm images at the westward and equatorward edge of the diffuse 630.0 nm patch nearly 2 minutes prior to expansion onset, suggesting a field‐aligned current of a substorm current wedge geometry. We conclude that the equatorward moving <jats:italic>λ</jats:italic> = 630.0 nm diffuse auroral patch was generated by processes associated with an earthward moving flow burst that formed prior to auroral substorm onset.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 36 (24), L24104-, 2009-12
American Geophysical Union (AGU)