With this archive, we can study solar activities in terms of the Sun's radiation in soft X-ray wavelengths. In this project, we will process the XRT/SCIA images taken from 2006 to date to derive the solar soft X-ray irradiance during this period. The student will learn how to process Hinode/XRT FITS data for quantitative analysis: selection of data files and area of interest, derivation of temperature and emission measure, calculation of the XRT irradiance in the physical unit comparable with other instruments. The student will also learn about data calibration applied to the original data to be used for analysis. Just like us, XRT instruments are aging during more than 12 years of operation in space. We should carefully separate the variation of the solar signals from that caused by the characteristic change of the instrument.
As a bonus, the student will have a few opportunities to watch and learn how an international satellite project like Hinode is operated. As one of US institutes participating the Hinode satellite operation, we have a duty week in July, in which we take control of the XRT observation.
Our team at MSU is currently developing a sounding rocket spectrometer called Full-sun Ultraviolet Rocket SpecTrometer(FURST). The student will also have an opportunity to interact with our research group at MSU and learn about their work.
Irradiance at SOHO : Is (at the L1 point : let R1 the distance from the Sun) Irradiance at Earth : Ie (at 1 AU, let R2 the distance from the Sun) When Is is measured, total Energy flux from the Sun: F_total = Is * 4*π*R12 Earth will receive this flux as Ie = F_total / 4*π*R22 This gives Ie = Is * R12 / R22 From R1 = 0.99 AU, R2=1 AU. We get Ie = 0.98 Is
dω1=Ar/r2 dω2=As/r2 Fs = Ls * As * dω1 = Ls * As * Ar / r2 Fr = Lr * Ar * dω2 = Lr * Ar * As / r2 if Fs = Fr then Ls = Lr : Radiance is invariant along the conserved flux.
Examples of Abstract