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Chromospheric LAyer SpectroPolarimeter (CLASP2)

机译:层大气分光光度计(CLASP2)

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The sounding rocket Chromospheric Lyman-Alpha SpectroPolarimeter (CLASP1) was launched on September 3rd, 2015, and successfully detected (with a polarization accuracy of 0.1 %) the linear polarization signals (Stokes Q and U) that scattering processes were predicted to produce in the hydrogen Lyman-alpha line (Lyman-α; 121.567 nm). Via the Hanle effect, this unique data set may provide novel information about the magnetic structure and energetics in the upper solar chromosphere. The CLASP 1 instrument was safely recovered without any damage and we have recently proposed to dedicate its second flight to observe the four Stokes profiles in the spectral region of the Mg Ⅱ h and k lines around 280 nm; in these lines the polarization signals result from scattering processes and the Hanle and Zeeman effects. Here we describe the modifications needed to develop this new instrument called the "Chromospheric LAyer SpectroPolarimeter" (CLASP2).
机译:探空火箭“莱曼-阿尔法”分光光度计(CLASP1)于2015年9月3日发射升空,成功探测到了偏振过程中会产生散射过程的线性偏振信号(斯托克斯Q和U)(偏振精度为0.1%)。氢Lyman-α线(Lyman-α; 121.567 nm)。通过Hanle效应,这个独特的数据集可以提供有关上部太阳色球层中的磁结构和高能学的新颖信息。 CLASP 1仪器已安全恢复,没有任何损坏,我们最近建议专门进行第二次飞行,以观察MgⅡh和k线在280 nm附近的光谱区域中的四个Stokes轮廓。在这些直线中,偏振信号是由散射过程以及Hanle和Zeeman效应产生​​的。在这里,我们描述了开发这种称为“大气层分光光度计”(CLASP2)的新仪器所需的修改。

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