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Properties Of The Suprathermal Heavy Ion Population Near 1 AU During Solar Cycles 23 And 24
被引:0
作者:
Dayeh, Maher A.
[1
]
Desai, Mihir I.
[1
,2
]
Ebert, Robert W.
[1
]
Mason, Glenn M.
[3
]
机构:
[1] Southwest Res Inst, 6220 Culebra Rd, San Antonio, TX 78023 USA
[2] Univ Texas San Antonio, Dept Phys & Astron, San Antonio, TX 78249 USA
[3] Johns Hopkins Univ, Appl Phys Lab, Johns Hopkins Rd, Laurel, MD 20723 USA
来源:
PROCEEDINGS OF THE FOURTEENTH INTERNATIONAL SOLAR WIND CONFERENCE (SOLAR WIND 14)
|
2016年
/
1720卷
基金:
美国国家科学基金会;
关键词:
ENERGETIC PARTICLE EVENTS;
INTERPLANETARY SHOCKS;
INTERACTION REGIONS;
SEED POPULATION;
COMMON SPECTRUM;
ACCELERATION;
WIND;
ABUNDANCES;
HELIOSPHERE;
D O I:
10.1063/1.4943838
中图分类号:
P3 [地球物理学];
P59 [地球化学];
学科分类号:
0708 ;
070902 ;
摘要:
Using measurements from the Advanced Composition Explorer/Ultra-Low Energy Isotope Spectrometer (ACE/ULEIS) near 1 AU, we surveyed the composition and spectra of heavy ions (He-through-Fe) during interplanetary quiet times from 1998 January 1 to 2014 December 31 at suprathermal energies between similar to 0.11 and similar to 1.28 MeV nucleon(-1). The selected time period covers the maxima of solar cycles 23 and 24 and the extended solar minimum in between. We find the following: (1) The number of quiet-hours in each year correlates well with the sunspot number, year 2009 was the quietest for about 90% of the time; (2) The composition of the quiet-time suprathermal heavy ion population (He-3, C-through-O, and Fe) correlates well with the level of solar activity, exhibiting SEP-like composition signatures during solar maximum, and CIR- or solar wind-like composition during solar minimum; (3) The heavy ion spectra at similar to 0.11-0.32 MeV nucleon(-1) exhibit suprathermal tails with power-law spectral indices ranging from 1.4 to 2.7. (4) Fe spectral indices get softer (steeper) from solar minimum of cycle 23 to solar cycle 24 maximum. These results imply that during IP quiet times and at energies above similar to 0.1 MeV nucleon(-1), the IP medium is dominated by material from prior solar and interplanetary events.
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