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首页> 外文期刊>Geophysical Research Letters >Precipitation of auroral protons in detached arcs - art. no. 1519
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Precipitation of auroral protons in detached arcs - art. no. 1519

机译:分离弧中极光质子的沉淀-艺术。没有。 1519

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摘要

1] Recent global-scale observations by the IMAGE-FUV instrument demonstrate the existence of regions of particle precipitation at sub-auroral latitudes on the dayside. The signature of this precipitation is seen infrequently, but when so, it is clear in all 3 channels of the FUV instrument. A conjugate hemisphere conjunction with the FAST satellite demonstrates the presence of precipitating protons and the notable absence of precipitating electrons in these arcs. With this knowledge, one can determine the mean energy and energy flux of the precipitating protons by intercomparison of the response in the three FUV channels. Assuming that the protons have a kappa energy distribution, the mean energy is found to be similar to 20 keV, with a peak in total energy flux of similar to1 mW/m(2)/sec, consistent with fits to the FAST ion measurements. These phenomena are observed mainly during times of high solar wind dynamic pressure and variable interplanetary magnetic field, and are associated with earlier nightside enhancements in the brightness and latitudinal extent of the proton aurora. [References: 17
机译:1] IMAGE-FUV仪器最近在全球范围内进行的观测表明,在白天,极光下纬度存在颗粒降水区域。这种沉淀的信号很少见,但在这种情况下,在FUV仪器的所有3个通道中都清晰可见。共轭半球与FAST卫星的结合证明了在这些弧中存在沉淀质子和明显不存在沉淀电子。有了这一知识,就可以通过比较三个FUV通道中的响应来确定沉淀质子的平均能量和能量通量。假设质子具有kappa能量分布,则发现平均能量类似于20 keV,总能量通量的峰值类似于1 mW / m(2)/ sec,与FAST离子测量的拟合一致。这些现象主要是在太阳风动压高和行星际磁场变化时观察到的,并且与较早的夜晚在质子极光的亮度和纬度范围内的增强有关。 [参考:17

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