Evolution of solar wind flows from the inner corona to 1 AU: constraints provided by SOHO UVCS and SWAN data

A. Bemporad, O. Katushkina, V. Izmodenov, D. Koutroumpa, E. Quémerais
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Abstract

The Sun modulates with the solar wind flow the shape of the whole Heliosphere interacting with the surrounding interstellar medium. Recent results from IBEX and INCA experiments, as well as recent measurements from Voyager 1 and 2, demonstrated that this interaction is much more complex and subject to temporal and heliolatitudinal variations than previously thought. These variations could be also related with the evolution of solar wind during its journey through the Heliosphere. Hence, understanding how the solar wind evolves from its acceleration region in the inner corona to the Heliospheric boundaries is very important.

In this work, SWAN Lyman-α full-sky observations from SOHO are combined for the very first time with measurements acquired in the inner corona by SOHO UVCS and LASCO instruments, to trace the solar wind expansion from the Sun to 1 AU. The solar wind mass flux in the inner corona was derived over one full solar rotation period in 1997, based on LASCO polarized brightness measurements, and on the Doppler dimming technique applied to UVCS Lyman-α emission from neutral H coronal atoms due to resonant scattering of chromospheric radiation. On the other hand, the SWAN Lyman-α emission (due to back-scattering from neutral H atoms in the interstellar medium) was analyzed based on numerical models of the interstellar hydrogen distribution in the heliosphere and the radiation transfer. The SWAN full-sky Lyman-α intensity maps are used for solving of the inverse problem and deriving of the solar wind mass flux at 1 AU from the Sun as a function of heliolatitude. First results from this comparison for a chosen time period in 1997 are described here, and possible future applications for Solar Orbiter data are discussed.

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从内日冕到1au的太阳风流演化:SOHO UVCS和SWAN数据提供的约束
太阳通过太阳风流来调节整个日球层的形状,并与周围的星际介质相互作用。IBEX和INCA实验的最新结果,以及旅行者1号和2号最近的测量结果表明,这种相互作用比以前认为的要复杂得多,而且受时间和日冕变化的影响。这些变化也可能与太阳风在穿越日球层过程中的演变有关。因此,了解太阳风如何从日冕内的加速区演变到日球层边界是非常重要的。在这部作品中,SWAN Lyman-αSOHO的全天观测首次与SOHO UVCS和LASCO仪器在日冕内获得的测量结果相结合,以追踪太阳风从太阳到1au的扩张。1997年,基于LASCO偏振亮度测量和应用于UVCS的多普勒调光技术,推导了一个完整太阳旋转周期内日冕内的太阳风质量通量。色球辐射共振散射引起的中性H日冕原子发射。另一方面,SWAN Lyman-α基于星际氢在日球层中的分布和辐射传输的数值模型,分析了星际氢在日球层中的反向散射。SWAN全天空莱曼-α强度图用于求解反问题,并推导出距离太阳1au处的太阳风质量通量随太阳经度的函数。本文描述了1997年选定时间段比较的第一个结果,并讨论了太阳轨道器数据未来可能的应用。
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