Faraday moments of the Southern Twenty-centimeter All-sky Polarization Survey (STAPS)

N. Raycheva, M. Haverkorn, S. Ideguchi, J. Stil, X. Sun, J. L. Han, E. Carretti, X. Y. Gao, A. Bracco, S. E. Clark, J. M. Dickey, B. Gaensler, A. Hill, T. Landecker, A. Ordog, A. Seta, M. Tahani, M. Wolleben
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Abstract

Faraday tomography of broadband radio polarization surveys enables us to study magnetic fields and their interaction with the interstellar medium (ISM). Such surveys include the Global Magneto-Ionic Medium Survey (GMIMS), which covers the northern and southern hemispheres at sim 300--1800 MHz. In this work, we used the GMIMS High Band South (1328--1768 MHz), also named the Southern Twenty-centimeter All-sky Polarization Survey (STAPS), which observes the southern sky at a resolution of 18arcmin . To extract the key parameters of the magnetized ISM from STAPS, we computed the Faraday moments of the tomographic data cubes. These moments include the total polarized intensity, the mean Faraday depth weighted by the polarized intensity, the weighted dispersion of the Faraday spectrum, and its skewness. We compared the Faraday moments to those calculated over the same frequency range in the northern sky (using the Dominion Radio Astrophysical Observatory, DRAO), in a strip of $360 that overlaps with STAPS coverage. We find that the total polarized intensity is generally dominated by diffuse emission that decreases at longitudes of $l The Faraday moments reveal a variety of polarization structures. Low-intensity regions at high latitudes usually have a single Faraday depth component. Due to its insufficiently large frequency coverage, STAPS cannot detect Faraday thick structures. Comparing the Faraday depths from STAPS to total rotation measures from extragalactic sources suggests that STAPS frequencies are high enough that the intervening ISM causes depolarization to background emission at intermediate and high Galactic latitudes. Where they overlap, the STAPS and DRAO surveys exhibit broad correspondence but differ in polarized intensity by a factor of sim 1.8.
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南方二十厘米全天空极化巡天(STAPS)的法拉第矩
宽带无线电极化巡天的法拉第层析成像使我们能够研究磁场及其与星际介质(ISM)的相互作用。这类勘测包括全球磁离子介质勘测(GMIMS),它覆盖南北半球,频率为 sim 300--1800 MHz。在这项工作中,我们使用的是 GMIMS 高频段南天(1328--1768 MHz),它也被命名为南二十厘米全天空极化巡天(STAPS),以 18arcmin 的分辨率观测南天。为了从 STAPS 中提取磁化 ISM 的关键参数,我们计算了层析成像数据立方体的法拉第矩。这些矩包括总偏振强度、按偏振强度加权的平均法拉第深度、法拉第谱的加权离散度及其偏斜度。我们将法拉第矩与在北部天空同一频率范围内计算出的法拉第矩进行了比较(利用多米尼昂射电天体物理观测台,DRAO),计算范围为 360 美元,与 STAPS 的覆盖范围重叠。我们发现,总的极化强度一般以弥散发射为主,在经度为 l 美元时,弥散发射会减弱。 法拉第矩揭示了多种极化结构。高纬度的低强度区域通常只有一个法拉第深度分量。由于其频率覆盖范围不够大,STAPS 无法探测到法拉第厚度结构。将 STAPS 的法拉第深度与银河系外源的总旋转测量结果进行比较,可以发现 STAPS 的频率足够高,以至于银河系中高纬度地区的干扰 ISM 会对背景发射产生去极化作用。在它们重叠的地方,STAPS 和 DRAO 勘测显示出广泛的对应关系,但偏振强度相差 1.8 倍。
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