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首页> 外文期刊>Annales Geophysicae >Solar cosmic rays during the extremely high ground level enhancement on 23 February 1956
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Solar cosmic rays during the extremely high ground level enhancement on 23 February 1956

机译:1956年2月23日,在极高的地面增强过程中,太阳宇宙射线

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The 23 February 1956 ground level enhancement of the solar cosmic rayintensity (GLE05) is the most famous among the proton events observed since1942. But we do not have a great deal of information on this event due tothe absence of solar wind and interplanetary magnetic field measurements atthat time. Furthermore, there were no X-Ray or gamma observations and theinformation on the associated flare is limited. Cosmic ray data was obtainedexclusively by ground level detectors of small size and in some cases ofa non-standard design. In the present work all available data from neutronmonitors operating in 1956 were analyzed, in order to develop a model of thesolar cosmic ray behavior during the event. The time-dependentcharacteristics of the cosmic ray energy spectrum, cosmic ray anisotropy,and differential and integral fluxes have been evaluated utilizing differentisotropic and anisotropic models. It is shown that the most outstandingfeatures of this proton enhancement were a narrow and extremely intense beamof ultra-relativistic particles arriving at Earth just after the onset andthe unusually high maximum solar particle energy. However, the contributionof this beam to the overall solar particle density and fluency was notsignificant because of its very short duration and small width. Our estimateof the integral flux for particles with energies over 100 MeV places thisevent above all subsequent. Perhaps the number of accelerated low energyparticles was closer to a record value, but these particles passed mainly tothe west of Earth. style="line-height: 20px;">Many features of this GLE are apparently explained by the peculiarity of theparticle interplanetary propagation from a remote (near the limb) source.The quality of the available neutron monitor data does not allow us to becertain of some details; these may be cleared up by the incorporation into theanalysis of data from muonic telescopes and ionization chambers operating atthat time.Keywords. Interplanatary physics (Cosmic rays; Energeticparticles) – Solar physics, astrophysics and astronomy(Flares and mass injections)
机译:自1942年以来观测到的质子事件中,最著名的是1956年2月23日的太阳宇宙射线强度(GLE05)地平面增强。但是由于当时没有太阳风和行星际磁场测量,因此我们没有关于此事件的大量信息。此外,没有X射线或伽玛射线观测,有关耀斑的信息有限。宇宙射线数据只能通过小尺寸的地平面探测器获得,在某些情况下是通过非标准设计获得的。在本工作中,分析了1956年运行的中子监测器的所有可用数据,以建立事件期间太阳宇宙射线行为的模型。利用不同的各向同性和各向异性模型对宇宙射线能谱,宇宙射线各向异性以及微分通量和积分通量的时变特征进行了评估。结果表明,这种质子增强的最显着特征是,超相对论粒子的一束狭窄且极强的光束在刚开始发生之后就到达了地球,并且异常高的最大太阳粒子能也到达了。但是,该光束对整个太阳能粒子密度和流度的贡献并不显着,因为其持续时间很短且宽度很小。我们对能量超过100 MeV的粒子的积分通量的估计将这一事件置于所有后续事件之上。加速的低能粒子的数量也许接近创纪录的值,但这些粒子主要通过地球的西部。 style =“ line-height:20px;”>显然,该GLE的许多特征可以通过以下方式解释:中子监测器数据的质量无法让我们确定某些细节;可以通过将当时运行的电子望远镜和电离室的数据合并到分析中来清除这些问题。 关键字。层间物理学(宇宙射线;高能粒子)–太阳物理学,天体物理学和天文学(耀斑和大量注入)

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