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Inverse problem in Ionospheric Science: Prediction of solar soft-X-ray spectrum from Very Low Frequency Radiosonde results

机译:电离层科学中的反问题:太阳软X射线的预测   来自极低频无线电探空仪结果的频谱

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摘要

X-rays and gamma-rays from astronomical sources such as solar flares aremostly absorbed by the Earth's atmosphere. Resulting electron-ion productionrate as a function of height depends on the intensity and wavelength of theinjected spectrum and therefore the effects vary from one source to another. Inother words, the ion density vs. altitude profile has the imprint of theincident photon spectrum. In this paper, we investigate whether we can invertthe problem uniquely by deconvolution of the VLF amplitude signal to obtain thedetails of the injected spectrum. We find that it is possible to do this up toa certain accuracy. Our method is useful to carry out a similar exercise toinfer the spectra of more energetic events such as the Gamma Ray Bursts (GRBs),Soft Gamma Ray Repeaters (SGRs) etc. by probing even the lower part of theatmosphere. We thus show that to certain extent, the Earth's atmosphere couldbe used as a gigantic detector of relatively strong events.
机译:来自天文来源(例如太阳耀斑)的X射线和伽马射线大部分被地球大气层吸收。所得到的作为高度函数的电子离子生产率取决于所注入光谱的强度和波长,因此,其影响在一个来源之间会有所不同。换句话说,离子密度与高度的关系图具有入射光子光谱的印记。在本文中,我们研究了是否可以通过对VLF幅度信号进行反卷积来唯一地反演该问题,以获得注入频谱的细节。我们发现可以做到一定精度。我们的方法可用于进行类似的练习,以探测甚至更低的大气层,从而推断出诸如伽玛射线暴(GRB),软伽玛射线中继器(SGR)等更多高能事件的光谱。因此,我们表明,在一定程度上,地球的大气层可以用作相对强事件的巨型探测器。

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