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Energy spectra of 50-keV to 20-MeV protons accelerated at corotating interaction regions at Ulysses

机译:50-keV到20-MeV质子的能谱在Ulysses的同向相互作用区域加速

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We analyze here the energy spectra of 50-keV to 20-MeV protons accelerated at corotating shocks observed at Ulysses in the southern heliosphere during 1992 and 1993. In general, our results are inconsistent with the predictions of two models based on diffusive shock acceleration theory (Fisk and Lee [1980] and Jones and Ellison [1991]). The main results are the following: (1) The relationships between the spectral indices and the shock compression ratio show significant departures from those predicted by the two models; the observed spectra are substantially harder than predicted; (2) the spectral indices at the reverse shocks depend strongly on the heliographic latitude of Ulysses; the hardest spectra are associated with strong quasi-perpendicular shocks observed between 20 deg S and 30 deg S; (3) the spectral indices at the reverse shocks are anticorrelated with the upstream plasma velocity V'_u in the de Hoffman-Teller frame of the shock; and (4) the spectral indices at the forward shocks show no dependence on either the shock parameters or the heliographic latitude. The latitudinal dependence of the reverse shock spectra is probably related to the tilt (approx 25 deg) of the heliospheric current sheet with respect to the solar equatorial plane during 1992 and 1993. The negative correlation between the spectral indices at the reverse shocks and V'_u indicates that the gradient drift mechanism plays a crucial role in accelerating particles at corotating interaction regions (CIRs). The differences in our observations at the forward and reverse shocks may be due to the presence of a more energetic seed population and an enhancement in the level of magnetic field fluctuations upstream of the trailing edges of the CIRs.
机译:我们在这里分析在1992年和1993年在南太阳圈的尤利西斯观测到的同向冲击中加速的50keV到20MeV质子的能谱。总体而言,我们的结果与基于扩散冲击加速理论的两个模型的预测不一致(Fisk and Lee [1980]和Jones and Ellison [1991])。主要研究结果如下:(1)光谱指数与冲击压缩比之间的关系与上述两个模型的预测值存在较大差异。观察到的光谱比预测的要难得多; (2)反向冲击时的光谱指数在很大程度上取决于尤利西斯的日射纬度;最坚硬的光谱与在20度和30度之间观察到的强烈的垂直振动有关。 (3)反向冲击波的频谱指数与该冲击波的德霍夫曼-泰勒框架中的上游等离子体速度V'_u反相关; (4)前向冲击波的频谱指数与冲击波参数或纬度无关。反向冲击光谱的纬度依赖性可能与1992年和1993年期间太阳流层相对于太阳赤道平面的倾斜度(大约25度)有关。反向冲击时的光谱指数与V'之间呈负相关。 _u表示梯度漂移机制在加速同向相互作用区域(CIR)处的粒子中起着至关重要的作用。我们在正向和反向冲击时观察到的差异可能是由于存在更高能量的种子种群,以及CIR后缘上游的磁场波动水平增强所致。

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