b emissions, focusing on the dusk-midnight sector of the auroral oval where the'/> SuperDARN E-region backscatter boundary in the dusk-midnight sector – tracer of equatorward boundary of the auroral oval
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SuperDARN E-region backscatter boundary in the dusk-midnight sector – tracer of equatorward boundary of the auroral oval

机译:黄昏至午夜扇形区的SuperDARN E区后向散射边界–极光椭圆的赤道边界示踪剂

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We compare the locations of the equatorward boundaries of SuperDARN E-region backscatter and H face="Symbol">b emissions, focusing on the dusk-midnight sector of the auroral oval where the proton aurora is statistically located equatorward of the discrete electron aurora. We show that, whenever both boundaries can be simultaneously identified, they are coincident. Our result complements earlier studies, which demonstrated the correspondence between the DMSP b2i boundary and both the equatorward boundary of the proton auroral oval (Donovan et al., 2002), and the equatorward boundary of SuperDARN E-region echoes (Jayachandran et al., 2002). Further, our result shows that, provided there is sufficient precipitating proton energy flux, the SuperDARN radars can be used to monitor the equatorward edge of the proton auroral oval.Key words. Ionosphere (auroral ionosphere; particle precipitation; ionospheric irregularities)
机译:我们比较了SuperDARN E区后向散射和H face =“ Symbol”> b 发射的赤道边界位置,重点是极光椭圆的黄昏至午夜部分,质子极光在统计上位于离散电子极光的赤道线上。我们表明,只要可以同时识别两个边界,它们就是一致的。我们的结果是对早期研究的补充,后者证明了DMSP b2i边界与质子极光椭圆的赤道边界(Donovan等,2002)以及SuperDARN E区回波的赤道边界之间的对应关系(Jayachandran等,2002)。 2002)。此外,我们的结果表明,只要有足够的质子能量通量沉淀,SuperDARN雷达就可以用于监测质子极光椭圆的赤道边缘。 关键词。 电离层(极光电离层;粒子沉淀;电离层不规则性)

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