Dominant Trends in Jupiter's H 3 + ${\mathbf{H}}_{\mathbf{3}}^{\mathbf{+}}$ Northern Aurora: II. Magnetospheric Mapping

IF 2.9 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Tom S. Stallard, Katie L. Knowles, Henrik Melin, Ruoyan Wang, Emma M. Thomas, Luke Moore, James O’Donoghue, Rosie E. Johnson, Steve Miller, John C. Coxon
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Abstract

Jupiter's auroral regions have previously been defined by broad-scale auroral structures, but these are typically obscured by the wide array of temporal variability observed at timescales between minutes and days, making it difficult to understand the underlying magnetospheric biases driving these brightness differences. Here, we follow on from an initial study of Jupiter's aurora, again utilizing a data set of > ${ >} $ 13,000 H 3 + ${\mathrm{H}}_{3}^{+}$ images of Jupiter mapped into latitude, longitude and local time, smoothed over tens of hours of integration and many days of observing. Having removed correlations between brightness and both magnetic field and planetary local time identified in the first study, we examine morphological changes in emission with both planetary and magnetic local time. We reveal that the H 3 + ${\mathrm{H}}_{3}^{+}$ main auroral emission is enhanced by a factor of three in the region mapping into the dusk magnetosphere. An additional strong auroral darkening is observed near noon, aligned with previous ultraviolet observations of an auroral discontinuity in this region, though this rotates duskward slightly in magnetic local time, as the ionospheric source mapping to this region moves duskward. The polar aurora contrasts with this strongly, showing brightness enhancement when the auroral pole points toward the dawn and dusk limbs. It also shows that the Dark region is fixed in local time, close to the dawnward edge of the polar region, while the Swirl region appears to match well with predictions from recent MHD models when the magnetic pole points toward dawn, but changes significantly at other magnetic pole directions.

Abstract Image

木星H 3 + ${\mathbf{H}}_{\mathbf{3}}^{\mathbf{+}}$北极光的主导趋势:II。磁性层的映射
木星的极光区域以前是由大尺度的极光结构定义的,但这些区域通常被在分钟到天的时间尺度上观察到的广泛的时间变化所掩盖,这使得很难理解驱动这些亮度差异的潜在磁层偏差。在这里,我们继续对木星极光的初步研究,再次利用>; ${>} $ 13,000 H 3 + ${\ mathm {H}}_{3}^{+}$ images的数据集木星被绘制成纬度、经度和当地时间,经过数十小时的整合和数天的观测,变得平滑。在消除了第一项研究中确定的亮度与磁场和行星当地时间之间的相关性之后,我们研究了发射与行星和磁场当地时间的形态变化。我们发现,在映射到黄昏磁层的区域,h3 + ${\ mathm {H}}_{3}^{+}$主极光发射增强了3倍。在正午附近观测到一个额外的强极光变暗,与之前紫外线观测到的这个区域的极光不连续一致,尽管它在磁地方时稍微向暗旋转,因为映射到这个区域的电离层源向暗移动。极地极光与此形成强烈对比,当北极点指向黎明和黄昏时,亮度会增强。它还表明,黑暗区域在当地时间是固定的,靠近极地地区的黎明边缘,而漩涡区域似乎与最近的MHD模型的预测相吻合,当磁极指向黎明时,但在其他磁极方向上发生了显著变化。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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