论文标题

深度多降限制了Reionisation时期21厘米功率光谱的深度限制,来自默奇森(Murchison

Deep multi-redshift limits on Epoch of Reionisation 21cm Power Spectra from Four Seasons of Murchison Widefield Array Observations

论文作者

Trott, Cathryn M., Jordan, C. H., Midgley, S., Barry, N., Greig, B., Pindor, B., Cook, J. H., Sleap, G., Tingay, S. J., Ung, D., Hancock, P., Williams, A., Bowman, J., Byrne, R., Chokshi, A., Hazelton, B. J., Hasegawa, K., Jacobs, D., Joseph, R. C., Li, W., Line, J. L. B, Lynch, C., McKinley, B., Mitchell, D. A., Morales, M. F., Ouchi, M., Pober, J. C., Rahimi, M., Takahashi, K., Wayth, R. B., Webster, R. L., Wilensky, M., Wyithe, J. S. B., Yoshiura, S., Zhang, Z., Zheng, Q.

论文摘要

我们从与Murchison Widefield阵列(MWA)观察到的回报时期(EOR)项目获得的四个季节的数据季节中计算了球形平均功率谱。我们在$ k = 0.07-3.0〜h $ mpc $^{ - 1} $上测量EOR功率频谱,RedShifts $ z = 6.5-8.7 $。 EOR0高频(3,340个观测值)的110小时的最大聚合得出的最低度量为(43〜mk)$^2 $ = 1.8 $ = 1.8 $ \ times $ 10 $^3 $^3 $^3 $ mk $^2 $ at $ k $ k $ = 0.14〜 $ h $ h $ h $ h $ h $ h $ h $ mpc $^mpc $^{ - 1} $^{ - $ z $ z = 6.5 $($ z = 6.5 $ plull and)使用实时系统校准和芯片管道来估计功率谱,我们从2013 - 2016年观察季节中选择了中央五个点的最佳观察结果,观察了三个独立的字段和两个频带。基于测量电离层活性的质量保证度量,这产生了13,591个2分钟的快照(453小时)。我们基于二维功率谱的前景主导和以EOR为主导的区域的功率进行另一个切割来删除较差的数据,从而将集合减少到12,569个观测值(419小时)。这些数据以20个观测值进行处理,以保留确定数据差的能力,并用于分析数据的演变和结构,而不是字段,频率和数据质量。随后,我们选择了最清洁的8,935个观测值(298小时的数据),以在不同的磁场,点和红移范围内形成集成的功率谱。

We compute the spherically-averaged power spectrum from four seasons of data obtained for the Epoch of Reionisation (EoR) project observed with the Murchison Widefield Array (MWA). We measure the EoR power spectrum over $k= 0.07-3.0~h$Mpc$^{-1}$ at redshifts $z=6.5-8.7$. The largest aggregation of 110 hours on EoR0 high-band (3,340 observations), yields a lowest measurement of (43~mK)$^2$ = 1.8$\times$10$^3$ mK$^2$ at $k$=0.14~$h$Mpc$^{-1}$ and $z=6.5$ (2$σ$ thermal noise plus sample variance). Using the Real-Time System to calibrate and the CHIPS pipeline to estimate power spectra, we select the best observations from the central five pointings within the 2013--2016 observing seasons, observing three independent fields and in two frequency bands. This yields 13,591 2-minute snapshots (453 hours), based on a quality assurance metric that measures ionospheric activity. We perform another cut to remove poorly-calibrated data, based on power in the foreground-dominated and EoR-dominated regions of the two-dimensional power spectrum, reducing the set to 12,569 observations (419 hours). These data are processed in groups of 20 observations, to retain the capacity to identify poor data, and used to analyse the evolution and structure of the data over field, frequency, and data quality. We subsequently choose the cleanest 8,935 observations (298 hours of data) to form integrated power spectra over the different fields, pointings and redshift ranges.

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