极低地球轨道PROBA-V/EPT和近赤道椭圆轨道Van Allen探测器/MagEIS对辐射带电子通量的观测

V. Pierrard, E. Botek, J. Ripoll, G. Reeves, S. Thaller
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引用次数: 0

摘要

利用欧空局PROBA-V卫星上的高能粒子望远镜(EPT)仪器,在820 km的极低地球轨道上对地磁风暴期间和之后外辐射带的电子通量进行了研究,并与在600 ~ 30600 km的低倾角椭圆轨道上运行的NASA范艾伦探测器上的MagEIS仪器的同步观测结果进行了比较。我们发现在中地球轨道观测到的赤道俘获电子通量比在近地轨道观测到的要高。在1兆电子伏以下,最大通量相差约2个数量级。然而,EPT超相对论通量(>2.4 MeV)远低于范艾伦探测器2.33 MeV的通量,相差4 ~ 5个数量级。我们还观察到,在安静时期,外层带是相当各向同性的,与内部带相反。在风暴期间(这里是2015年6月23日的大风暴),在LEO和MEO观测到的通量下降和通量增加呈现非常相似的形状。
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Observations of Electron Fluxes in the Radiation Belts with PROBA-V/EPT at Polar Low Earth Orbit and Van Allen Probes/MagEIS at Near Equatorial Elliptical Orbit
The electron fluxes in the outer radiation belt during and after geomagnetic storms were investigated using the EPT (Energetic Particle Telescope) instrument on board the ESA PROBA-V satellite at a polar LEO (Low Earth Orbit) at 820 km of altitude and compared with simultaneous observations of the instrument MagEIS on board the NASA Van Allen Probes circulating on a low inclination elliptical orbit ranging from 600 to 30 600 km.We find that the equatorial trapped electron fluxes observed at MEO (Medium Earth Orbit) are higher than at LEO. Below 1 MeV, maximal fluxes differ by ~2 orders of magnitude. However, the EPT ultra-relativistic flux (>2.4 MeV) is much lower than the Van Allen Probes flux at 2.33 MeV, by 4 to 5 orders of magnitude. We also observe that the outer belt is quite isotropic during quiet times, contrary to the inner belt. During storms (here, the big storm of 23 June 2015), the dropout and flux increase observed at LEO and MEO present very similar shapes.
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