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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Solar wind alpha particles and heavy ions in the inner heliosphere observed with MESSENGER
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Solar wind alpha particles and heavy ions in the inner heliosphere observed with MESSENGER

机译:用MESSENGER观测到的太阳风中的Alpha粒子和内部日球中的重离子

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摘要

[1] The Fast Imaging Plasma Spectrometer (FIPS) on the MErcury Surface, Space ENvironment, GEochemistry, and Ranging (MESSENGER) spacecraft has made the first in situ measurements of solar wind plasma in the inner heliosphere since the Helios 1 and 2 spacecraft in the 1980s. Although the core of the solar wind velocity distribution is obstructed by the spacecraft sunshade, a data analysis technique has been developed that recovers both bulk and thermal speeds to 10% accuracy and provides the first measurements of solar wind heavy ions (mass per charge >2 amu/e) at heliocentric distances within 0.5 AU. Solar wind alpha particles and heavy ions appear to have similar mean flow speeds at values greater than that of the protons by approximately 70% of the Alfvén speed. From an examination of the thermal properties of alpha particles and heavier solar wind ions, we find a ratio of the temperature of alpha particles to that of protons nearly twice that of previously reported Helios observations, though still within the limits of excessive heating of heavy ions observed spectroscopically close to the Sun. Furthermore, examination of typical magnetic power spectra at the orbits of MESSENGER and at 1 AU reveals the lack of a strong signature of local resonant ion heating, implying that a majority of heavy ion heating could occur close to the Sun. These results demonstrate that the solar wind at ~0.3 AU is a blend of the effects of wave-particle interactions occurring in both the solar corona and the heliosphere.
机译:[1]自从Helios 1和2航天器进入水银表面,太空环境,地球化学和测距(MESSENGER)航天器以来,快速成像等离子体光谱仪(FIPS)首次对内部太阳圈中的太阳风等离子体进行了原位测量。 1980年代。尽管太阳风速度分布的核心受到航天器遮阳帘的阻碍,但已经开发了一种数据分析技术,该技术可以将体积速度和热速度恢复到10%的精度,并提供了太阳风重离子的首次测量值(每电荷质量> 2 amu / e)在0.5 AU以内的日心距离。太阳风中的α粒子和重离子似乎具有相似的平均流速,其值比质子的平均流速高大约Alfvén速度的70%。通过对α粒子和较重的太阳风离子的热性质的检查,我们发现α粒子与质子的温度之比几乎是以前报道的Helios观测值的两倍,尽管仍在重离子过度加热的范围内在光谱上接近太阳观察到。此外,对MESSENGER轨道和1 AU处的典型磁功率谱的检查表明,缺乏局部共振离子加热的强烈信号,这意味着大部分重离子加热可能会在太阳附近发生。这些结果表明,〜0.3 AU处的太阳风是在日冕和日球层中发生的波粒相互作用的综合作用。

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