首页> 外文期刊>The Astrophysical journal >DECONVOLUTION OF DIRECTLY PRECIPITATING AND TRAP-PRECIPITATING ELECTRONS IN SOLAR FLARE HARD X-RAYS. III. YOHKOH HARD X-RAY TELESCOPE DATA ANALYSIS
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DECONVOLUTION OF DIRECTLY PRECIPITATING AND TRAP-PRECIPITATING ELECTRONS IN SOLAR FLARE HARD X-RAYS. III. YOHKOH HARD X-RAY TELESCOPE DATA ANALYSIS

机译:在太阳耀斑硬X射线中直接析出和陷阱捕捉电子的去卷积。三, YOHKOH硬X射线望远镜数据分析

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We analyze the footpoint separation d and flux asymmetry A of magnetically conjugate double foot- point sources in hard X-ray images from the Yohkoh Hard X-Ray Telescope (HXT). The data set of 54 solar flares includes all events simultaneously observed with the Compton Gamma Ray Observatory (CGRO) in high time resolution mode. From the CGRO data we deconvolved the direct-precipitation and trap-precipitation components previously (in Paper II). Using the combined measurements from CGRO and HXT, we develop an asymmetric trap model that allows us to quantify the relative fractions of four different electron components, i.e., the ratios of direct-precipitating (q_p1, q_p2) and trap- precipitating electrons (q_T1, q_T2) at both magnetically conjugate footpoints. We find mean ratios of q_p1 = 0.14 ± 0.06, q_p2 = 0.26 ± 0.10, and q_T = q_T1 + q_T2 = 0.60 ± 0.13. We assume an isotropic pitch- angle distribution at the acceleration site and double-sided trap precipitation (q_T2/q_T1 = q_p2/q_P1) to determine the conjugate loss-cone angles ( α_1 = 42°±11°and α_2= 52°± 10°) and magnetic mirror ratios at both footpoints (R_1 = 1.6, . . . , 4.0 and R_2=1.3,...,2.5). From the relative displacement of footpoint sources we also measure altitude differences of hard X-ray emission at different energies, Which are found to decrease systematically with higher energies, with a statistical height difference of h_Lo -h_M1=980 ± 250 km and h_M1 - h_M2 = 310 ± 300 km between the three lower HXT energy channels (Lo, M1, M2).
机译:我们分析了来自Yohkoh硬X射线望远镜(HXT)的硬X射线图像中的磁共轭双足点源的足点间距d和磁通不对称A。 54个太阳耀斑的数据集包括在康普顿伽玛射线天文台(CGRO)上以高时间分辨率模式同时观测到的所有事件。根据CGRO数据,我们先前对卷积的直接降水和圈闭降水进行了反卷积(在论文II中)。利用CGRO和HXT的组合测量结果,我们开发了一个不对称陷阱模型,该模型使我们能够量化四种不同电子组分的相对分数,即直接沉淀电子(q_p1,q_p2)和陷阱沉淀电子(q_T1, q_T2)在两个磁共轭脚点处。我们发现q_p1 = 0.14±0.06,q_p2 = 0.26±0.10和q_T = q_T1 + q_T2 = 0.60±0.13的平均比率。我们假设加速点处的各向同性俯仰角分布和双侧陷阱降水(q_T2 / q_T1 = q_p2 / q_P1)来确定共轭损失锥角(α_1= 42°±11°和α_2= 52°±10角)和两个脚点处的磁镜比率(R_1 = 1.6,...,4.0和R_2 = 1.3,...,2.5)。从脚点源的相对位移,我们还测量了不同能量下硬X射线发射的高度差,发现高能量下该强度会系统地减小,其统计高度差为h_Lo -h_M1 = 980±250 km和h_M1- h_M2在三个较低的HXT能量通道(Lo,M1,M2)之间= 310±300 km。

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