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arXiv 2307.02445astro-ph.SR
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量化宁静太阳光球中的坡印廷通量

Quantifying Poynting flux in the Quiet Sun Photosphere

Dennis Tilipman, Maria Kazachenko, Benoit Tremblay, Ivan Milic, Valentin Martinez Pillet, Matthias Rempel

AI总结:

本文利用Sunrise/IMaX观测和MURaM模拟研究宁静太阳光球坡印廷通量,比较FLCT与DeepVel速度推断方法,提出新的方位角消歧方法,并结合PDFI_SS电场反演评估其对色球和日冕加热的贡献。

摘要:

坡印廷通量是磁能通量,负责太阳大气中色球层和日冕的加热。它被定义为电场和磁场的叉积,在理想磁流体力学条件下可以用磁场和等离子体速度来表示。坡印廷通量已针对活动区和谱斑进行了计算,但由于分辨率效应和偏振噪声,在宁静太阳中估算它仍然具有挑战性。然而,随着即将到来的DKIST能力,这些估算将变得比以往任何时候都更加可行。在这里,我们研究Sunrise/IMaX观测和MURaM模拟中的宁静太阳坡印廷通量。我们探索了两种从观测中推断横向速度的方法——FLCT和一种基于神经网络的方法DeepVel——并表明在小尺度宁静太阳流的背景下,DeepVel是更合适的方法。我们研究了方位角模糊对坡印廷通量估算的影响,并描述了一种新的方位角消歧方法。最后,我们使用两种方法获得电场。第一种方法依赖于理想化欧姆定律,而第二种是一种最先进的感应电场反演方法PDFI_SS。我们将所得的坡印廷通量值与色球层和日冕能量损失的理论估算值进行比较,发现一些坡印廷通量估算值足以匹配这些损失。利用MURaM模拟,我们表明光球坡印廷通量随光学深度显著变化,并且存在一种观测偏差,由于未考虑的剪切项贡献而导致坡印廷通量被低估。

英文摘要:

Poynting flux is the flux of magnetic energy, which is responsible for chromospheric and coronal heating in the solar atmosphere. It is defined as a cross product of electric and magnetic fields, and in ideal MHD conditions it can be expressed in terms of magnetic field and plasma velocity. Poynting flux has been computed for active regions and plages, but estimating it in the quiet Sun (QS) remains challenging due to resolution effects and polarimetric noise. However, with upcoming DKIST capabilities, these estimates will become more feasible than ever before. Here, we study QS Poynting flux in Sunrise/IMaX observations and MURaM simulations. We explore two methods for inferring transverse velocities from observations - FLCT and a neural network based method DeepVel - and show DeepVel to be the more suitable method in the context of small-scale QS flows. We investigate the effect of azimuthal ambiguity on Poynting flux estimates, and we describe a new method for azimuth disambiguation. Finally, we use two methods for obtaining the electric field. The first method relies on idealized Ohm's law, whereas the second is a state-of-the-art inductive electric field inversion method PDFI SS. We compare the resulting Poynting flux values with theoretical estimates for chromospheric and coronal energy losses and find that some of Poynting flux estimates are sufficient to match the losses. Using MURaM simulations, we show that photospheric Poynting fluxes vary significantly with optical depth, and that there is an observational bias that results in underestimated Poynting fluxes due to unaccounted shear term contribution.

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