论文标题

确定IO Decametric排放的光束:一种远程诊断,用于探测IO-Jupiter相互作用

Determining the beaming of Io decametric emissions : a remote diagnostic to probe the Io-Jupiter interaction

论文作者

Lamy, L., Colomban, L., Zarka, P., Prangé, R., Marques, M. S., Louis, C., Kurth, W., Cecconi, B., Girard, J., Griessmeier, J. -M., Yerin, S.

论文摘要

我们研究了朱诺/波,Nan \ c Cay Decameter Array和Nenufar观察到的11个IO-Jupiter DeTametric(IO-DAM)排放的横梁。使用最新的磁场模型和三种方法来定位主动IO通量管(IFT),我们准确地定位了辐射程序,并确定其发射角$θ$从局部磁场向量。这些方法使用(i)IFT赤道铅角度的更新模型,(ii)木星Aurorae和(iii)多点无线电测量的紫外线(UV)图像。然后,从源电子电子的动能$ e_ {e - } $从$θ$中推断出在回旋子梅尔不稳定性的框架内。从方法(II,III)中实现的活性IFT的精确位置可用于测试有效的圆环等离子体密度。同时进行无线电/紫外线观测表明,多个IO-DAM弧与多个紫外线相关联,并提供了与跨性跨性束紫外线相关的IO-DAM弧的第一个直接证据。多点无线电观察结果在各种高度,时间和半球处探测IO-DAM的来源。总体而言,$θ$从$ 75^\ circ-80^\ circ $降低到$ 70^\ circ-75^\ circy $ 10-40 $ MHz,在北半球的值略大,并且独立于时间(或IO的函数),$θ$的频率(高度)变化。它的几个程度的不确定性主要由主动IFT经度的误差所占据主导地位。 $ e_ {e - } $的推断值也随着时间和时间的函数而变化。在11个调查案例中,它们的范围为3至16个KEV,$ 6.6 \ pm2.7 $ kev的平均水平。

We investigate the beaming of 11 Io-Jupiter decametric (Io-DAM) emissions observed by Juno/Waves, the Nan\c cay Decameter Array and NenuFAR. Using an up-to-date magnetic field model and three methods to position the active Io Flux Tube (IFT), we accurately locate the radiosources and determine their emission angle $θ$ from the local magnetic field vector. These methods use (i) updated models of the IFT equatorial lead angle, (ii) ultraviolet (UV) images of Jupiter's aurorae and (iii) multi-point radio measurements. The kinetic energy $E_{e-}$ of source electrons is then inferred from $θ$ in the framework of the Cyclotron Maser Instability. The precise position of the active IFT achieved from methods (ii,iii) can be used to test the effective torus plasma density. Simultaneous radio/UV observations reveal that multiple Io-DAM arcs are associated with multiple UV spots and provide the first direct evidence of an Io-DAM arc associated with a trans-hemispheric beam UV spot. Multi-point radio observations probe the Io-DAM sources at various altitudes, times and hemispheres. Overall, $θ$ varies a function of frequency (altitude), by decreasing from $75^\circ-80^\circ$ to $70^\circ-75^\circ$ over $10-40$ MHz with slightly larger values in the northern hemisphere, and independently varies as a function of time (or longitude of Io). Its uncertainty of a few degrees is dominated by the error on the longitude of the active IFT. The inferred values of $E_{e-}$ also vary as a function of altitude and time. For the 11 investigated cases, they range from 3 to 16 keV, with a $6.6\pm2.7$ keV average.

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