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首页> 外文期刊>The Astrophysical journal >Radio Astronomical Constraints on Coronal Heating by High-Frequency Alfvén Waves
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Radio Astronomical Constraints on Coronal Heating by High-Frequency Alfvén Waves

机译:高频Alfvén波对日冕加热的射电天文约束

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It has been suggested that the heating of the solar corona and the acceleration of the solar wind to their observed values are due to high-frequency (1 to several hundred Hertz) magnetohydrodynamic (MHD) waves. This suggestion circumvents well-established difficulties with heating and acceleration by observed, low-frequency (milliHertz) MHD waves. There is no widely accepted mechanism for damping the low-frequency waves, and their observed amplitude throughout the inner heliosphere is insufficient to account for observed solar wind properties. By contrast, the alleged high-frequency waves would not be detected by radio propagation observations (specifically Faraday rotation observations) hitherto conducted, so the amplitude of these waves would appear to be a free parameter for the theories. The purpose of this paper is to show that these putative waves might reveal themselves through another observable radio propagation phenomenon, Faraday screen depolarization. Faraday screen depolarization is a reduction of the observed degree of linear polarization of an extended, polarized radio source when viewed through a medium (here referred to as a screen) in which the Faraday rotation varies in a random fashion. Expressions for Faraday screen depolarization are extracted from the literature and calculations appropriate to the solar corona and inner solar wind are made. Depending on the exact properties of the high-frequency turbulence, a detectable (i.e. ~5%-20%) depolarization could result. We present six polarimetric observations at a frequency of 1465 MHz of polarized sources observed close to the Sun with the Very Large Array radio telescope in 1997. These observations show no detectable depolarization and rule out some turbulence models. The existing observations are far from being definitive in ruling out high-frequency turbulence with the required properties. However, additional observations, particularly undertaken at lower radio frequencies, could furnish far more restrictive limits.
机译:已经提出,太阳日冕的加热和太阳风向其观测值的加速是由于高频(1至几百赫兹)磁流体动力学(MHD)波引起的。该建议通过观察到的低频(毫赫兹)MHD波来规避加热和加速方面公认的困难。没有衰减低频波的广泛接受的机制,并且它们在整个内部太阳圈的观测振幅不足以说明观测到的太阳风特性。相比之下,迄今为止进行的无线电传播观测(特别是法拉第旋转观测)将无法检测到所谓的高频波,因此这些波的振幅似乎是理论的一个自由参数。本文的目的是表明这些推定的波可能通过另一种可观察到的无线电传播现象即法拉第屏幕去极化来揭示自己。法拉第屏幕去极化是通过法拉第旋转随机变化的介质(此处称为屏幕)观察时,扩展的极化无线电源的线性极化程度的降低。从文献中提取了法拉第屏幕去极化的表达式,并进行了适合日冕和内部太阳风的计算。取决于高频湍流的确切特性,可能会导致可检测到的去极化(约5%-20%)。我们在1997年使用甚大阵列射电望远镜在靠近太阳的地方观测了极化源在1465 MHz频率上的六次极化观测。这些观测结果显示没有可检测到的去极化,并且排除了一些湍流模型。在排除具有所需特性的高频湍流方面,现有的观察结果还远远不够明确。但是,更多的观察,尤其是在较低的射频下进行的观察,可能会提供更多的限制。

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