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TINY PORES OBSERVED BY HINODE/SOLAR OPTICAL TELESCOPE

机译:日报/太阳能望远镜观察到的微小孔

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The study of pores, small penumbraless sunspots, can give us a chance to understand how strong magnetic fields interact with convective motions in the photosphere. For a better understanding of this interaction, we investigate the temporal variation of several tiny pores smaller than 2''. These pores were observed by the Solar Optical Telescope on board Hinode on 2006 December 29. We have analyzed the high-resolution spectropolarimetric (SP) data and the G-band filtergrams taken during the observation. Magnetic flux density and Doppler velocities of the pores are estimated by applying the center-of-gravity method to the SP data. The horizontal motions in and around the pores are tracked by adopting the nonlinear affine velocity estimator method to the G-band filter images. As a result, we found the following. (1) The darkness of the pores is positively correlated with the magnetic flux density. (2) Downflows always exist inside and around the pores. (3) The speed of downflows inside the pores is negatively correlated with their darkness. (4) The pores are surrounded by strong downflows. (5) Brightness changes of the pores are correlated with the divergence of mass flow (correlation coefficient 0.9). (6) The pores in the growing phase are associated with the converging flow pattern and the pores in the decay phase with the diverging flow pattern. Our results support the idea that a pore grows as the magnetic flux density increases due to the convergence of ambient mass flow and it decays with the decrease of the flux density due to the diverging mass flow.
机译:对毛孔,无半影状的小黑子的研究可以使我们有机会了解强磁场如何与光层中的对流运动相互作用。为了更好地了解这种相互作用,我们研究了几个小于2''的细孔的时间变化。这些孔隙是由2006年12月29日在Hinode上的太阳光学望远镜观测到的。我们分析了高分辨率的光谱极化(SP)数据和观测期间获得的G波段滤光片。孔隙的磁通密度和多普勒速度是通过将重心法应用于SP数据来估算的。通过对G波段滤波图像采用非线性仿射速度估计方法来跟踪孔中和孔周围的水平运动。结果,我们发现以下内容。 (1)孔的暗度与磁通密度呈正相关。 (2)孔内和孔周围始终存在下流。 (3)孔内向下流动的速度与其暗度成负相关。 (4)孔隙被强烈的向下流动所包围。 (5)孔的亮度变化与质量流的发散有关(相关系数> 0.9)。 (6)处于生长期的孔隙与汇流型态相关,而处于衰落阶段的孔隙与流型型态相关。我们的结果支持这样一种观点,即孔隙随着环境质量流的收敛而随着磁通密度的增加而增长,并且随着质量流的扩散而随着磁通密度的降低而衰减。

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