Connerney J E, Baron R, Satoh T, Owen T
Science. 1993 Nov 12;262(5136):1035-8. doi: 10.1126/science.262.5136.1035.
The electrodynamic interaction between lo and the Jovian magnetosphere drives currents to and from the planet's ionosphere, where H(3)(+) emission is excited. Direct images of this phenomenon were obtained with the ProtoCAM infrared camera at the National Aeronautics and Space Administration's 3-m Infrared Telescope Facility. The emissions are localized to the instantaneous foot of the lo flux tube, approximately 8 degrees equatorward of the more intense auroral H(3)(+) emission associated with higher magnetic latitudes. The foot of the lo flux tube leads that of (undisturbed) model magnetic field lines passing through lo by 15 degrees to 20 degrees in longitude and is less visible in the northern hemisphere at longitudes where the surface magnetic field strength is greatest. These data favor the unipolar inductor model of the lo interaction and provide insight into the source location and generation of Jovian decameter radio emission.
木卫一与木星磁层之间的电动力相互作用驱动电流往返于行星的电离层,在那里H(3)(+)发射被激发。利用美国国家航空航天局3米红外望远镜设施的ProtoCAM红外相机获得了这一现象的直接图像。这些发射集中在木卫一磁通量管的瞬时足迹处,位于与较高磁纬度相关的更强极光H(3)(+)发射向赤道方向约8度处。木卫一磁通量管的足迹在经度上比穿过木卫一的(未受干扰的)模型磁力线的足迹超前15度至20度,并且在表面磁场强度最大处的北半球经度上不太明显。这些数据支持木卫一相互作用的单极感应模型,并为木星十米射电发射的源位置和产生提供了见解。