Science. 1986 Jul 4;233(4759):102-6. doi: 10.1126/science.233.4759.102.
Within distances to Uranus of about 6 x 10(6) kilometers (inbound) and 35 x 10(6) kilometers (outbound), the planetary radio astronomy experiment aboard Voyager 2 detected a wide variety of radio emissions. The emission was modulated in a period of 17.24 +/- 0.01 hours, which is identified as the rotation period of Uranus' magnetic field. Of the two poles where the axis of the off-center magnetic dipole (measured by the magnetometer experiment aboard Voyager 2) meets the planetary surface, the one closer to dipole center is now located on the nightside of the planet. The radio emission generally had maximum power and bandwidth when this pole was tipped toward the spacecraft. When the spacecraft entered the nightside hemisphere, which contains the stronger surface magnetic pole, the bandwidth increased dramatically and thereafter remained large. Dynamically evolving radio events of various kinds embedded in these emissions suggest a Uranian magnetosphere rich in magnetohydrodynamic phenomena.
在距离天王星约 6×10^6 公里(向内)和 35×10^6 公里(向外)的范围内,旅行者 2 号上的行星射电天文实验探测到了各种各样的射电辐射。该辐射的调制周期为 17.24±0.01 小时,这被确定为天王星磁场的自转周期。在两个磁极中,磁强计实验测量的偏心磁偶极子的轴与行星表面相交,距离偶极子中心更近的那个磁极现在位于行星的夜晚侧。当这个磁极指向航天器时,无线电辐射通常具有最大功率和带宽。当航天器进入包含较强表面磁极的夜晚半球时,带宽急剧增加,此后一直保持较大。这些辐射中嵌入的各种动态演化的无线电事件表明,天王星的磁层中富含磁流体动力学现象。