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On the Heating of the Solar Corona and the Acceleration of the Low-Speed Solar Wind by Acoustic Waves Generated in Corona

机译:关于太阳能电弧的加热和低速加速的研究   电晕产生的声波产生的太阳风

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摘要

We investigate possibilities of solar coronal heating by acoustic wavesgenerated not at the photosphere but in the corona, aiming at heating in themid- to low-latitude corona where the low-speed wind is expected to come from.Acoustic waves of period tau ~ 100s are triggered by chromosphericreconnection, one model of small scale magnetic reconnection events recentlyproposed by Sturrock. These waves having a finite amplitude eventually formshocks to shape sawtooth waves (N-waves), and directly heat the surroundingcorona by dissipation of their wave energy. Outward propagation of the N-wavesis treated based on the weak shock theory, so that the heating rate can beevaluated consistently with physical properties of the background coronalplasma without setting a dissipation length in an ad hoc manner. We constructcoronal structures from the upper chromosphere to the outside of 1AU forvarious inputs of the acoustic waves having a range of energy flux of F_{w,0} =(1-20) times 10^5 erg cm^{-2} s^{-1} and a period of tau = 60-300s. The heatingby the N-wave dissipation effectively works in the inner corona and we findthat the waves of F_{w,0} >= 2 times 10^5 erg cm^{-2} s^{-1} and tau >= 60scould maintain peak coronal temperature, T_{max} > 10^6 K. The model could alsoreproduce the density profile observed in the streamer region. However, due toits short dissipation length, the location of T_{max} is closer to the surfacethan the observation, and the resultant flow velocity of the solar wind islower than the observed profile of the low-speed wind. The cooperations withother heating and acceleration sources with the larger dissipation length areinevitable to reproduce the real solar corona.
机译:我们研究了不是在光球而是在电晕中产生的声波对太阳日冕加热的可能性,旨在在中低纬度电晕中加热,预计低速风来自该电晕.tau〜100s的声波是由色球层重新连接触发,这是Sturrock最近提出的一种小规模磁性重新连接事件的模型。这些具有有限振幅的波最终形成节拍以成形锯齿波(N波),并通过消散其波能直接加热周围的电晕。基于弱冲击理论处理的N波的向外传播,因此可以与背景冠状体的物理特性一致地评估加热速率,而无需专门设置耗散长度。对于声波的各种输入,我们构造了从上层色球层到1AU外部的冠状结构,其能量通量范围为F_ {w,0} =(1-20)乘以10 ^ 5 erg cm ^ {-2} s ^ {-1},tau周期= 60-300s。 N波耗散产生的热量有效地作用于内部电晕,我们发现F_ {w,0}> = 2乘以10 ^ 5 erg cm ^ {-2} s ^ {-1}和tau> = 60维持最高冠冕温度T_ {max}> 10 ^ 6K。该模型还可以再现在拖缆区域观察到的密度分布。但是,由于其短的耗散长度,因此T_ {max}的位置比观测值更靠近表面,并且太阳风的合成流速比观测到的低速风的流速低。与其他具有较大耗散长度的加热和加速源的配合不可避免地要重现真实的日冕。

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    Suzuki, Takeru Ken;

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  • 年度 2002
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