首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >The effects of lunar surface plasma absorption and solar wind temperature anisotropies on the solar wind proton velocity space distributions in the low-altitude lunar plasma wake
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The effects of lunar surface plasma absorption and solar wind temperature anisotropies on the solar wind proton velocity space distributions in the low-altitude lunar plasma wake

机译:月球表面等离子体吸收和太阳风温度各向异性对低空月球等离子体尾流中太阳风质子速度空间分布的影响

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We study the solar wind proton velocity space distribution functions on the lunar nightside at low altitudes (~100 km) above the lunar surface using a three-dimensional hybrid plasma solver, when the Moon is in the unperturbed solar wind. When the solar wind encounters a passive obstacle, such as the Moon, without any strong magnetic field and no atmosphere, solar wind protons that impact the obstacle's surface are absorbed and removed from the velocity space distribution functions. We show first that a hybrid model of plasma is applicable to study the low-altitude lunar plasma wake by comparing the simulation results with observations. Then we examine the effects of a solar wind bi-Maxwellian velocity space distribution function and the lunar surface plasma absorption on the solar wind protons' velocity space distribution functions and their entry in the direction parallel to the interplanetary magnetic field lines into the low-altitude lunar wake. We present a backward Liouville method for particle-in-cell solvers that improves velocity space resolution. The results show that the lunar surface plasma absorption and anisotropic solar wind velocity space distributions result in substantial changes in the solar wind proton distribution functions in the low-altitude lunar plasma wake, modifying proton number density, velocity, and temperature there. Additionally, a large temperature anisotropy is found at close distances to the Moon on the lunar nightside as a consequence of the lunar surface plasma absorption effect.
机译:当月球处于不受干扰的太阳风中时,我们使用三维混合等离子体解算器研究了在月球表面上方低海拔(〜100 km)处低空(〜100 km)的月球夜间太阳风的质子速度空间分布函数。当太阳风遇到诸如月球之类的被动障碍物时,没有任何强磁场且没有大气层,撞击障碍物表面的太阳风质子将被吸收并从速度空间分布函数中移除。我们首先表明,通过将模拟结果与观测值进行比较,等离子体的混合模型可用于研究低空月球等离子体唤醒。然后,我们研究了太阳风双麦克斯韦速度空间分布函数和月球表面等离子体吸收对太阳风质子速度空间分布函数的影响以及它们在平行于行星际磁场线的方向上进入低空的影响。月球醒来。我们提出了一种向后的Liouville方法,用于改进单元格中的粒子速度空间分辨率。结果表明,月球表面等离子体吸收和各向异性的太阳风速度空间分布导致低空月球等离子体尾流中太阳风质子分布函数的实质性变化,从而改变了那里的质子数密度,速度和温度。另外,由于月球表面等离子吸收效应,在月球夜边距月球很近的距离处发现了较大的温度各向异性。

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