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Discrete Aurora at Mars: Dependence on Upstream Solar Wind Conditions

机译:离散在火星极光:上游的依赖太阳风条件

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Discrete aurora at Mars, characterized by their small spatial scale and tendency to form near strong crustal magnetic fields, are emissions produced by particle precipitation into the Martian upper atmosphere. Since 2014, Mars Atmosphere and Volatile EvolutioN's (MAVEN's) Imaging Ultraviolet Spectrograph (IUVS) has obtained a large collection of UV discrete aurora observations during its routine periapsis nightside limb scans. Initial analysis of these observations has shown that, near the strongest crustal magnetic fields in the southern hemisphere, the IUVS discrete aurora detection frequency is highly sensitive to the interplanetary magnetic field (IMF) clock angle. However, the role of other solar wind properties in controlling the discrete aurora detection frequency has not yet been determined. In this work, we use the IUVS discrete aurora observations, along with MAVEN observations of the upstream solar wind, to determine how the discrete aurora detection frequency varies with solar wind dynamic pressure, IMF strength, and IMF cone angle. We find that, outside of the strong crustal field region (SCFR) in the southern hemisphere, the aurora detection frequency is relatively insensitive to the IMF orientation, but significantly increases with solar wind dynamic pressure, and moderately increases with IMF strength. Interestingly however, although high solar wind dynamic pressures cause more aurora to form, they have little impact on the brightness of the auroral emissions. Alternatively, inside the SCFR, the detection frequency is only moderately dependent on the solar wind dynamic pressure, and is much more sensitive to the IMF clock and cone angles. In the SCFR, aurora are unlikely to occur when the IMF points near the radial or anti-radial directions when the cone angle (arccos(B_x/|B|)) is less than 30° or between 120° and 150°. Together, these results provide the first comprehensive characterization of how upstream solar wind conditions affect the formati
机译:离散的极光在火星上,他们的特征小空间的规模和形式附近的倾向强烈的地壳磁场,排放由粒子沉淀到火星高层大气。大气与挥发性演化(MAVEN的)紫外成像光谱仪(IUVS)获得了大量的紫外线离散的极光观察在常规近拱点夜侧肢体扫描。观测表明,最强的附近地壳磁场在南部半球,IUVS离散极光检测频率是高度敏感的行星际磁场(IMF)时钟角。然而,其他太阳风属性的作用在控制离散极光检测频率尚未确定。工作中,我们使用IUVS离散的极光观察,连同MAVEN的观察上游太阳风,来确定检测频率随离散极光太阳风动态压力,国际货币基金组织的力量,国际货币基金组织的锥角。强烈的地壳场地区(SCFR)南半球,极光检测频率是国际货币基金组织(IMF)相对不敏感取向,但显著增加太阳风动态压力,和适度增加国际货币基金组织的力量。然而,尽管高太阳风动态压力导致更多的极光,对极光的亮度影响不大排放。检测频率只是适度的依赖太阳风动态压力,太多对国际货币基金组织时钟和锥角更加敏感。SCFR,极光时不太可能发生国际货币基金组织点附近径向或anti-radial方向当锥角(arccos B (bx / | |)小于30°、120°和150°之间。在一起,这些结果提供第一上游的综合表征影响formati太阳风条件

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