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arXiv 1102.0003astro-ph.SR
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年轻太阳太阳风及其与地球古磁层相互作用的模拟

Modeling the Young Sun's Solar Wind and its Interaction with Earth's Paleomagnetosphere

M. Glenn Sterenborg, Ofer Cohen, Jeremy J. Drake, Tamas I. Gombosi

摘要:

我们提出了一个集中的参数研究太阳风磁层相互作用的年轻的太阳和地球,$~3.5$ Ga ago,依赖于磁流体动力学(MHD)模拟的太阳风和磁层。通过模拟静止的年轻太阳和太阳风,我们可以将MHD模拟结果传播到地球磁层,并得到一个物理上真实的太阳强迫。我们评估了年轻的太阳风对日冕基底密度、太阳黑子位置和磁场强度、偶极磁场强度以及太阳自转周期变化的敏感程度。从这个分析中,我们得到了一个合理的太阳风条件的古磁层可能受到的范围。文献中的尺度关系表明,年轻的太阳会有不同于现在太阳的质量通量。我们评估如何与上述因素的质量通量的变化,并确定这个和其他几个关键的太阳和磁层变量的重要性,就其对古磁层的影响。我们改变了太阳风的速度,密度,行星际磁场强度和方向,以及地球的偶极子磁场强度和倾斜在一些稳态的情况下,是年轻的太阳-地球相互作用的代表。这项研究是为了更全面地了解太阳-地球相互作用对行星大气演变的影响而进行的第一步。

英文摘要:

We present a focused parameter study of solar wind - magnetosphere interaction for the young Sun and Earth, $~3.5$ Ga ago, that relies on magnetohydrodynamic (MHD) simulations for both the solar wind and the magnetosphere. By simulating the quiescent young Sun and its wind we are able to propagate the MHD simulations up to Earth's magnetosphere and obtain a physically realistic solar forcing of it. We assess how sensitive the young solar wind is to changes in the coronal base density, sunspot placement and magnetic field strength, dipole magnetic field strength and the Sun's rotation period. From this analysis we obtain a range of plausible solar wind conditions the paleomagnetosphere may have been subject to. Scaling relationships from the literature suggest that a young Sun would have had a mass flux different from the present Sun. We evaluate how the mass flux changes with the aforementioned factors and determine the importance of this and several other key solar and magnetospheric variables with respect to their impact on the paleomagnetosphere. We vary the solar wind speed, density, interplanetary magnetic field strength and orientation as well as Earth's dipole magnetic field strength and tilt in a number of steady-state scenarios that are representative of young Sun-Earth interaction. This study is done as a first step of a more comprehensive effort towards understanding the implications of Sun-Earth interaction for planetary atmospheric evolution.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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