2004
DOI: 10.1029/2003ja010073
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Core ion interactions with BB ELF, lower hybrid, and Alfvén waves in the high‐latitude topside ionosphere

Abstract: [1] We present simultaneous observations of ion distribution functions and plasma waves in the high-latitude topside ionosphere (500-1000 km) near local midnight during substorm activation. Using a new instrument, the Suprathermal Ion Imager (SII), we are able to explore two-dimensional ion distribution functions with unprecedented resolution in time (93 s À1 ) and energy, focusing on the lowest-energy core (<1 eV) population and suprathermal extensions thereof. The GEODESIC sounding rocket flew through region… Show more

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Cited by 29 publications
(45 citation statements)
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“…Notice that this requirement is not only applicable to regions where ξ T = T e0 /T i0 > 1 (or, equivalently, T e0 > T i0 ), but also to those where T e0 < T i0 . Table 1 lists some plasma parameters in auroral regions where T e0 > T i0 , calculated from measurements by the GEODESIC rocket (Burchill et al, 2004), the Freja satellite , and the FAST satellite (Ergun, 1999), respectively. By contrast, in most magnetosphic plasmas (especially encountering some extreme situations like, e.g., substorms), ξ T lies between 1/12 and 1/3, as reported by, e.g., AMPTE/IRM and Cluster observations in the Earth's central plasma sheet, the sheet boundary layers, and magnetosheath (Baumjohann, 1993;Phan et al, 1994;Lavraud, 2009).…”
Section: A Preliminary Simulation To Observationsmentioning
confidence: 99%
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“…Notice that this requirement is not only applicable to regions where ξ T = T e0 /T i0 > 1 (or, equivalently, T e0 > T i0 ), but also to those where T e0 < T i0 . Table 1 lists some plasma parameters in auroral regions where T e0 > T i0 , calculated from measurements by the GEODESIC rocket (Burchill et al, 2004), the Freja satellite , and the FAST satellite (Ergun, 1999), respectively. By contrast, in most magnetosphic plasmas (especially encountering some extreme situations like, e.g., substorms), ξ T lies between 1/12 and 1/3, as reported by, e.g., AMPTE/IRM and Cluster observations in the Earth's central plasma sheet, the sheet boundary layers, and magnetosheath (Baumjohann, 1993;Phan et al, 1994;Lavraud, 2009).…”
Section: A Preliminary Simulation To Observationsmentioning
confidence: 99%
“…Table 1. Some typical plasma parameters in auroral plasmas measured by the Geodesic rocket (Burchill et al, 2004), the Freja satellite , and the FAST satellite (Ergun, 1999 Appendix A…”
Section: A Preliminary Simulation To Observationsmentioning
confidence: 99%
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“…Wahlund et al, 1998;Knudsen et al, 1998;Kintner et al, 2000;Lund et al, 2000;Lynch et al, 2002;Hamrin et al, 2002;Bogdanova et al, 2004;Burchill et al, 2004;Backrud et al, 2005;Tam et al, 2005). The term BB-ELF has been used to refer to different frequency ranges by different authors, but generally it covers a frequency range from below the ion cyclotron frequency to above the ion plasma frequency.…”
Section: Introductionmentioning
confidence: 99%
“…Using data from the GEODESIC sounding rocket, Burchill et al (2004) used the SII to resolve strongly heated ion populations confined within filamentary density cavities only 20 m in diameter, and to track ion flow velocity variations within a 3 Hz shear Alfvén wave. Burchill et al (2010) In this paper we provide a technical description of the e-POP SEI instrument in Sect.…”
mentioning
confidence: 99%