Correlation between energetic ion enhancements and heliospheric current sheet crossings in the outer heliosphere
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- J. D. Richardson
- Center for Space Research Massachusetts Institute of Technology Cambridge Massachusetts USA
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- E. C. Stone
- Division of Physics, Mathematics, and Astronomy California Institute of Technology Pasadena California USA
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- A. C. Cummings
- Division of Physics, Mathematics, and Astronomy California Institute of Technology Pasadena California USA
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- J. C. Kasper
- Center for Space Research Massachusetts Institute of Technology Cambridge Massachusetts USA
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- M. Zhang
- Department of Physics and Space Sciences Florida Institute of Technology Melbourne Florida USA
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- L. F. Burlaga
- Laboratory for Solar and Space Physics NASA Goddard Space Flight Center Greenbelt Maryland USA
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- N. F. Ness
- Bartol Research Institute University of Delaware Newark Delaware USA
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- Y. Liu
- Center for Space Research Massachusetts Institute of Technology Cambridge Massachusetts USA
書誌事項
- 公開日
- 2006-11
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2006gl027578
- 公開者
- American Geophysical Union (AGU)
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説明
<jats:p>Voyagers 1 and 2 observed highly‐variable beams of energetic ions in the foreshock region upstream of the termination shock (TS). At Voyager 2 (V2), the ion intensities are generally not related to the plasma properties. At Voyager 1 (V1), the beams are often coincident with crossings of the heliospheric current sheet (HCS). The V1 intensity peaks occur when the HCS is crossed from negative to positive magnetic polarities and V1 is within a few AU of the TS. Two mechanisms are considered: current sheet drift and streaming of ions from the TS along magnetic field lines which are parallel to the HCS. The current sheet drift hypothesis predicts that enhancements observed at V2 will occur when the HCS is crossed in the opposite direction, from positive to negative magnetic polarity, since V2 is at southern heliolatitudes.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 33 (21), 1-, 2006-11
American Geophysical Union (AGU)
