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首页> 外文期刊>The Astrophysical journal >Voyager 1 and 2 Observations of Magnetic Fields and Associated Cosmic-Ray Variations from 2000 through 2001: 60-87 AU
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Voyager 1 and 2 Observations of Magnetic Fields and Associated Cosmic-Ray Variations from 2000 through 2001: 60-87 AU

机译:2000年至2001年旅行者1和2的磁场和相关宇宙射线变化的观测:AU 60-87

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We consider the cosmic and heliospheric magnetic field observations made during the years 2000 and 2001 when Voyager 1 (V1) moved from 76.1 to 87 AU at a heliographic latitude of approximately 345 and Voyager 2 (V2) moved from 59.8 to 69 AU at a heliographic latitude of approximately -255. A global merged interaction region (GMIR) containing intense fluctuating magnetic fields was observed by V2 and V1 at ≈61 and ≈78 AU, respectively, during 2000. This GMIR produced the first steplike decrease in the cosmic-ray intensity observed in the distant heliosphere during solar cycle 23. The GMIR and the steplike decrease in cosmic-ray intensity occurred later at V1 than at V2, the time delay being approximately the propagation time of the GMIR from V2 to V1 at the solar wind speed. A spherically symmetric MHD model, with data from 1 AU as input, predicts the GMIR that caused the step decrease at V2 during the year 2000, consistent with a view that the GMIR had the form of a quasi-spherical shell. The radial extent of the GMIR was ≈13-20 AU at V2 and ≈28 AU at V1, indicating a deviation of the shape of the GMIR from spherical symmetry. It is possible that, when the trailing edge of the GMIR moved past V1, the leading part of the GMIR was in the heliosheath beyond the termination shock, if the termination shock was between 80 and 100 AU. The GMIR consisted of a cluster of magnetic field strength enhancements by a factor of ≈2 on average. Decreases in the cosmic-ray intensity were observed by V2 and by V1 (starting at the end of 2000 and the beginning of 2001, respectively), and regions containing intense magnetic fields, which were probably parts of a second GMIR, caused them. Throughout the years 2000 and 2001, both V1 and V2 observed a correlation between changes in the cosmic-ray intensity and the magnetic field strength that are qualitatively described by the "CR-B relation." Thus, the GMIRs remain effective modulation agents as they travel through the most distant regions observed to date.
机译:我们考虑在2000年和2001年进行的宇宙和日球磁场观测,当时旅行者1(V1)在大约345度的纬度上从76.1移至87 AU,旅行者2(V2)在一次纬度从纬度55.9移至69 AU。纬度约为-255。在2000年期间,V2和V1分别在≈61和≈78AU处观测到一个包含强烈波动磁场的全局合并相互作用区域(GMIR)。该GMIR产生了在遥远的日球层观测到的宇宙射线强度的第一个阶梯状下降在太阳周期23期间,GMIR和宇宙射线强度的阶梯式下降在V1发生的时间比在V2发生的时间晚,该时间延迟大约是GMIR在太阳风速下从V2到V1的传播时间。一个球形对称MHD模型,以1 AU的数据作为输入,预测GMIR导致2000年V2阶跃减小,这与认为GMIR具有准球形壳的观点一致。 GMIR的径向范围在V2为≈13-20AU,在V1为≈28AU,表明GMIR的形状与球对称性存在偏差。如果终止冲击在80到100 AU之间,则当GMIR的后沿移过V1时,GMIR的前导部分可能会在终止冲击之外的螺旋鞘中。 GMIR由一组磁场强度增强平均组成≈2倍。 V2和V1(分别从2000年底和2001年初开始)观察到了宇宙射线强度的下降,并且由强磁场(可能是第二次GMIR的一部分)引起的。在2000年和2001年期间,V1和V2都观测到宇宙射线强度变化和磁场强度之间的相关性,用“ CR-B关系”定性地描述了这种变化。因此,当GMIR穿过迄今为止观察到的最远的区域时,它们仍然是有效的调节剂。

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