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Ulysses COSPIN observations of cosmic rays and solar energetic particles from the South Pole to the North Pole of the Sun during solar maximum

机译:尤利西斯·COSPIN在太阳最大时观测到从太阳的南极到太阳的北极的宇宙射线和太阳高能粒子

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摘要

In 2000–2001 Ulysses passed from the south to the north polar regions of the Sun in the inner heliosphere, providing a snapshot of the latitudinal structure of cosmic ray modulation and solar energetic particle populations during a period near solar maximum.  Observations from the COSPIN suite of energetic charged particle telescopes show that latitude variations in the cosmic ray intensity in the inner heliosphere are nearly non-existent near solar maximum, whereas small but clear latitude gradients were observed during the similar phase of Ulysses’ orbit near the 1994–95 solar minimum. At proton energies above ~10 MeV and extending up to 70 MeV, the intensities are often dominated by Solar Energetic Particles (SEPs) accelerated near the Sun in association with intense solar flares and large Coronal Mass Ejections (CMEs). At lower energies the particle intensities are almost constantly enhanced above background, most likely as a result of a mix of SEPs and particles accelerated by interplanetary shocks. Simultaneous high-latitude Ulysses and near-Earth observations show that most events that produce large flux increases near Earth also produce flux increases at Ulysses, even at the highest latitudes attained. Particle anisotropies during particle onsets at Ulysses are typically directed outwards from the Sun, suggesting either acceleration extending to high latitudes or efficient cross-field propagation somewhere inside the orbit of Ulysses. Both cosmic ray and SEP observations are consistent with highly efficient transport of energetic charged particles between the equatorial and polar regions and across the mean interplanetary magnetic fields in the inner heliosphere.Interplanetary physics (cosmic rays) – Solar physics, astrophysics and astronomy (energetic particles; flares and mass ejections)
机译:在2000–2001年期间,尤利西斯号从太阳的南极向南极内部的北半球穿过,为宇宙射线调制和太阳高能粒子群的纬度结构快照提供了一个近似太阳最大值的时期。来自COSPIN高能带电粒子望远镜套件的观测结果表明,在太阳最大值附近,几乎不存在内太阳圈内宇宙射线强度的纬度变化,而在尤里西斯轨道的相似相附近,观测到了小而清晰的纬度梯度。 1994–95年最低日照。在质子能量高于〜10 MeV并延伸至> 70 MeV时,强度通常受太阳附近加速的太阳高能粒子(SEP)的控制,并伴有强烈的太阳耀斑和大的日冕物质抛射(CME)。在较低的能量下,粒子强度几乎总是在背景以上不断提高,这很可能是由于SEP和行星际撞击加速了粒子混合的结果。同时进行的高纬度尤利西斯和近地观测表明,即使在达到最高纬度的情况下,大多数在地球附近产生较大通量增加的事件也会在尤利西斯产生通量增加。尤利西斯粒子爆发期间的粒子各向异性通常是从太阳向外指向的,这表明加速度可能扩展到高纬度,或者是尤利西斯轨道内部某处的有效交叉场传播。宇宙射线和SEP观测都与高能带电粒子在赤道和极地区域之间以及跨内部日球的平均行星际磁场中的高效传输相一致。行星际物理学(宇宙射线)–太阳物理学,天体物理学和天文学(高能粒子) ;耀斑和大量喷射)

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