Inner magnetospheric heavy ion composition during high-speed stream-driven storms

被引:9
|
作者
Forster, D. R. [1 ]
Denton, M. H. [1 ,2 ]
Grande, M. [3 ]
Perry, C. H. [4 ]
机构
[1] Univ Lancaster, Dept Phys, Lancaster LA1 4YB, England
[2] Space Sci Inst, Boulder, CO USA
[3] Aberystwyth Univ, Inst Math & Phys, Aberystwyth, Dyfed, Wales
[4] Rutherford Appleton Lab, Didcot OX11 0QX, Oxon, England
关键词
Ring Current; Ions; CIR; HSS; RADIATION BELT ELECTRONS; SOLAR-WIND STREAMS; RELATIVISTIC ELECTRONS; GEOSYNCHRONOUS ORBIT; GEOMAGNETIC STORMS; MAGNETIC STORMS; CYCLOTRON WAVES; ACCELERATION; PLASMA; DISTRIBUTIONS;
D O I
10.1002/jgra.50292
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Ion composition data, taken by the Combined Release and Radiation Effects Satellite Magnetospheric Ion Composition Spectrometer instrument, are investigated across eight high-speed solar wind-stream-driven storms (HSSs) during 1991. The HSSs are identified using solar wind data from OMNI alongside geomagnetic indices, and the behavior of ions in the energy range 31.2-426.0keV is investigated. A case study of the single HSS event that occurred on 30 July 1991 is performed, and superposed epoch analyses of five events are conducted. The data show evidence of a local minimum (dropout) in the flux and partial number density of ionic species H+, He+, He++, and O+ close to the onset of magnetospheric convection. The flux and number density rapidly fall and then recover over a period of hours. The initial rapid recovery in number density is observed to consist primarily of lower-energy ions. As the number density reaches its maximum, the ions show evidence of energization. Heavy ion-to-proton ratios are observed to decrease substantially during these HSS events.
引用
收藏
页码:4066 / 4079
页数:14
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