论文标题
用端到端仪器模拟校准锣磁图III:比较,校准和结果
Calibrating GONG Magnetograms with End-to-end Instrument Simulation III: Comparison, Calibration, and Results
论文作者
论文摘要
这是三篇论文中的最后一篇,描述了使用其测量过程的和端到端模拟对锣的校准的“绝对”校准。仿真以MURAM 3D MHD DATACUBE开头,并以Gong观察到的相应磁场值的“合成磁图”结束。我们通过将合成磁场测量值与产生它们的穆拉姆磁场值进行比较来确定校准。前两篇论文描述了锣测量过程(仪器和数据处理),我们对其的模拟以及磁图比较和校准的理论。在本文中,我们解决了有关校准的一些最终要点,将所有这些工作结合到一组校准曲线中,然后考虑结果。我们还回顾了前两篇论文的结果,以进行参考。我们的校准表明,锣磁图低估了弱通量在磁盘中心附近的2倍以上,但是随着视线接近肢体,该因子降至约1。对这些结果的普遍性的初步研究表明,其他工具将以类似的方式受到影响。我们还发现,以前的磁摄影比较的某些差异是仪器分辨率的伪影,这些伪影不能反映固有的校准差异,并且测量值比有时想象的要相似。这些结果直接适用于太阳风预测模型精确度的问题,尤其是在寻找在1 AU处预测的太阳风磁通量与当前卫星任务原位测得的值之间的常见差异的原因。
This is the last of three papers describing an `absolute' calibration of the GONG magnetograph using and end-to-end simulation of its measurement process. The simulation begins with a MURaM 3D MHD datacube and ends with a `synthetic magnetogram' of the corresponding magnetic field values as they would be observed by GONG. We determine a calibration by comparing the synthetic magnetic field measurements with the MURaM magnetic field values that produced them. The previous two papers have described the GONG measurement process (both instrument and data processing), our simulation of it, and the theory of magnetogram comparison and calibration. In this paper, we address some final points on calibration, combine all of this work into a set of calibration curves, and consider the results. We also review the results of the previous two papers for locality of reference. Our calibration indicates that GONG magnetograms underestimate weak flux by a factor of over 2 near disk center, but that factor decreases to about 1 as the line-of-sight approaches the limb. A preliminary investigation of the generalizability of these results suggests other instruments will be affected in a similar way. We also find that some differences in previous magnetograph comparisons are artifacts of instrumental resolution which do not reflect an intrinsic calibration difference, and the measurements are more similar than sometimes thought. These results are directly applicable to question of solar wind prediction model accuracies, particularly in the search for the cause of the common discrepancy between predicted solar wind magnetic flux at 1 AU and values measured in situ by current satellite missions.