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首页> 外文期刊>The Astrophysical journal >EXAMINING THE EFFECT OF THE MAP-MAKING ALGORITHM ON OBSERVED POWER ASYMMETRY IN WMAP DATA
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EXAMINING THE EFFECT OF THE MAP-MAKING ALGORITHM ON OBSERVED POWER ASYMMETRY IN WMAP DATA

机译:检查制图算法对WMAP数据中观察到的功率不对称性的影响

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摘要

We analyze first-year data of WMAP to determine the significance of asymmetry in summed power between arbitrarily defined opposite hemispheres. We perform this analysis on maps that we create ourselves from the time-ordered data, using software developed independently of the WMAP team. We find that over the multipole range l = [2, 64], the significance of asymmetry is ~10~(-4), a value insensitive to both frequency and power spectrum. We determine the smallest multipole ranges exhibiting significant asymmetry and find 12, including l = [2, 3] and [6, 7], for which the significance →0. Examination of the 12 ranges indicates both an improbable association between the direction of maximum significance and the ecliptic plane (significance ~0.01) and that contours of least significance follow great circles inclined relative to the ecliptic at the largest scales. The great circle for l = [2, 3] passes over previously reported preferred axes and is insensitive to frequency, while the great circle for l = [6, 7] is aligned with the ecliptic poles. We examine how changing map-making parameters, e.g., foreground masking, affects asymmetry. Only one change appreciably reduces asymmetry: asymmetry at large scales (l ≤ 7) is rendered insignificant if the magnitude of the WMAP dipole vector (368.11 km s~(-1)) is increased by ≈1 -3 σ (≈2-6 km s~(-1)). While confirmation of this result requires the recalibration of the time-ordered data, such a systematic change would be consistent with observations of frequency-independent asymmetry. We conclude that the use of an incorrect dipole vector, in combination with a systematic or foreground process associated with the ecliptic, may help to explain the observed power asymmetry.
机译:我们分析了WMAP的第一年数据,以确定任意定义的相对半球之间的总和不对称性的重要性。我们使用独立于WMAP团队开发的软件,在按时间顺序数据创建的地图上执行此分析。我们发现在多极范围l = [2,64]上,不对称的意义为〜10〜(-4),该值对频率和功率谱均不敏感。我们确定表现出显着不对称性的最小多极范围,并找到12,包括l = [2,3]和[6,7],其意义→0。对这12个范围的检验表明,最大显着性方向与黄道平面之间的可能性不大(显着性〜0.01),而最小显着性的轮廓则遵循相对于黄道最大比例的大圆。 l = [2,3]的大圆圈越过先前报告的首选轴,并且对频率不敏感,而l = [6,7]的大圆圈与黄极对齐。我们研究了更改地图制作参数(例如前景遮罩)如何影响不对称性。只有一个变化可以明显减少不对称性:如果WMAP偶极子向量(368.11 km s〜(-1))的幅度增加≈1-3-σ(≈2-6),则大比例的不对称性(l≤7)变得微不足道。公里s〜(-1))。虽然要确认此结果需要重新校准按时间顺序排列的数据,但这种系统性更改将与独立于频率的不对称现象一致。我们得出结论,使用不正确的偶极子矢量以及与黄道相关的系统或前景过程可能有助于解释观测到的功率不对称。

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