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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Radial diffusion of relativistic electrons into the radiation belt slot region during the 2003 Halloween geomagnetic storms
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Radial diffusion of relativistic electrons into the radiation belt slot region during the 2003 Halloween geomagnetic storms

机译:相对论电子在2003年万圣节地磁风暴中向辐射带缝隙区域的径向扩散

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摘要

A study was undertaken to estimate the radial diffusion timescale, τ LL , for relativistic electrons (2–6 MeV) to diffuse into the slot region due to drift-resonance with Pc5 ULF waves (2–10 mHz) on 29 October 2003. Large amplitude ULF waves were observed by ground-based magnetometer arrays to penetrate deep into the slot region (L 2–3) starting at 0600 UT and maximising (~200 nT p-p) between 0930–1630 UT. Around the same time, the SAMPEX PET instrument measured an over two orders of magnitude increase in relativistic (2–6 MeV) electron flux levels in ~24 hours within the slot region. The ground-based D-component magnetic power spectral densities (PSDδB ) for 29 October were estimated for six latitudinally spaced ground stations covering L ~ 2.3–4.3 for an observed ULF wave with central frequency ~4 mHz. The PSDδB values were used to calculate the in situ equatorial poloidal wave electric field power spectral densities (PSDδEm ) using a standing Alfvén wave model. The radial diffusion coefficients, D LL , were estimated using the PSDδEm values. The fastest τ LL were 3–5 hours at L > 4, while τ LL initially increased with decreasing L-value below L 4; peaking at L 3 with τ LL ~ 12–24 hours with PSDδEm estimated using a wave frequency bandwidth between Δf = 1 mHz and Δf = 2.5 mHz. The τ LL over the L-range L ~ 2.3–3.3 were consistent with the timescales observed by SAMPEX for the increase in relativistic fluxes in the slot region on 29 October. The authors believe that this is the first example of the ULF wave drift-resonance with relativistic electrons explaining a radiation belt slot region filling event.
机译:进行了一项研究,以估计相对论电子(2–6 MeV)由于在2003年10月29日与Pc5 ULF波(2–10 mHz)的漂移共振而扩散到缝隙区域中的径向扩散时间尺度τLL。大地面磁力计阵列观察到振幅为ULF的波,从0600 UT开始深入到缝隙区域(L 2–3),并在0930–1630 UT之间最大化(〜200 nT pp)。大约在同一时间,SAMPEX PET仪器在狭缝区域内约24小时内测量出相对论(2–6 MeV)电子通量水平增加了两个数量级。对于中心频率约为4 mHz的观察到的ULF波,估计了六个纬向分布的地面站的10月29日的地面D分量磁功率谱密度(PSDδB),范围为L〜2.3-4.3。 PSDδB值用于使用站立Alfvén波模型来计算原地赤道极谱波电场功率谱密度(PSDδEm)。使用PSDδEm值估算径向扩散系数D LL。当L> 4时,最快的τLL为3-5小时,而τLL最初随着L值降至L 4以下而增加。在ΔLL〜12–24小时的L 3处达到峰值,而PSDδEm使用在Δf= 1 mHz和Δf= 2.5 mHz之间的波带宽估计。 L范围L〜2.3-3.3上的τLL与10月29日狭缝区域相对论通量增加的SAMPEX观测到的时间尺度一致。作者认为,这是具有相对论性电子的ULF波漂移共振的第一个例子,解释了辐射带缝隙区域填充事件。

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