ENERGETIC ATOMIC AND MOLECULAR-IONS OF IONOSPHERIC ORIGIN OBSERVED IN DISTANT MAGNETOTAIL FLOW-REVERSAL EVENTS

被引:40
作者
CHRISTON, SP
GLOECKLER, G
WILLIAMS, DJ
MUKAI, T
MCENTIRE, RW
JACQUEY, C
ANGELOPOULOS, V
LUI, ATY
KOKUBUN, S
FAIRFIELD, DH
HIRAHARA, M
YAMAMOTO, T
机构
[1] JOHNS HOPKINS UNIV,APPL PHYS LAB,LAUREL,MD 21042
[2] INST SPACE & ASTRONAUT SCI,SAGAMIHARA,KANAGAWA 229,JAPAN
[3] NAGOYA UNIV,SOLAR TERR ENVIRONM LAB,TOKYOKAWA 442,JAPAN
[4] UNIV TOKYO,DEPT EARTH & PLANETARY PHYS,TOKYO 113,JAPAN
[5] NASA,GODDARD SPACE FLIGHT CTR,EXTRATERR PHYS LAB,GREENBELT,MD 20771
关键词
D O I
10.1029/94GL02095
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Energetic atomic (O+1 and N+1) and molecular (O-2(+1), NO+1, and N-2(+1)) ions of ionospheric origin were observed in Earth's magnetotail at X similar to -146 R(E) during two plasma sheet sunward/tailward now-reversal events measured by instruments on the GEOTAIL spacecraft. These events were associated with concurrent ground-measured geomagnetic disturbance intensification at auroral- and mid-latitudes (Kp = 7(-)). Energetic ions in the sunward-component and tailward flows were from both the solar wind and ionosphere. Plasma and energetic ions participated in the flows. During tailward flow, ionospheric origin ion abundance ratios at similar to 200-900 km/s in the rest frame were N+1/O+1 = similar to 25-30% and (O-2(+1), NO+1, and N-2(+1))/O+1 = similar to 1-2%. We argue that tailward flow most likely initiated similar to 80-100 R(E) tailward of Earth and molecular ions were in the plasma sheet prior to geomagnetic intensification onset.
引用
收藏
页码:3023 / 3026
页数:4
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