论文标题

CMB及其仪表不变性的单极波动

Monopole Fluctuation of the CMB and its Gauge Invariance

论文作者

Baumgartner, Sandra, Yoo, Jaiyul

论文摘要

观察到的CMB温度各向异性的标准理论描述$θ(\ hat n)$是量规依赖性的。但是,众所周知,量规模式仅限于单极,而较高的角多尔斯$θ_l$($ l \ geq1 $)是量规不变的。过去已经尝试了几次尝试正确定义单极波动,但是由于红外差异,单极功率$ C_0 $的结果值是无限的。红外差异源于均匀的引力对单极波动的贡献,违反了等效原理。在这里,我们介绍观察到的CMB温度各向异性的规格不变理论描述,并计算单极力量$ C_0 = 1.66 \ times10^{ - 9} $中的$ CDM型号。虽然标准计算中的量规依赖性源于今天定义背景CMB温度$ \ bar t $的高表面的歧义,但实际上它是定义的,并且是基本宇宙学参数之一。我们认为,一旦选择了宇宙学参数,就可以明确地从观察到的CMB温度的角度平均来推断单极波动,从而使其成为模型依赖性的“可观察”。采用简单的各向异性形成的近似值,我们为观察到的CMB温度各向异性提供了量规不变的分析表达,以研究CMB单极波动,并取消了均匀的重力潜在贡献。

The standard theoretical description $Θ(\hat n)$ of the observed CMB temperature anisotropies is gauge-dependent. It is, however, well known that the gauge mode is limited to the monopole and the higher angular multipoles $Θ_l$ ($l\geq1$) are gauge-invariant. Several attempts have been made in the past to properly define the monopole fluctuation, but the resulting values of the monopole power $C_0$ are infinite due to the infrared divergences. The infrared divergences arise from the contribution of the uniform gravitational potential to the monopole fluctuation, in violation of the equivalence principle. Here we present the gauge-invariant theoretical description of the observed CMB temperature anisotropies and compute the monopole power $C_0=1.66\times10^{-9}$ in a $Λ$CDM model. While the gauge-dependence in the standard calculations originates from the ambiguity in defining the hypersurface for the background CMB temperature $\bar T$ today, it is in fact well defined and one of the fundamental cosmological parameters. We argue that once the cosmological parameters are chosen, the monopole fluctuation can be unambiguously inferred from the angle-average of the observed CMB temperature, making it a model-dependent ''observable''. Adopting simple approximations for the anisotropy formation, we derive a gauge-invariant analytical expression for the observed CMB temperature anisotropies to study the CMB monopole fluctuation and the cancellation of the uniform gravitational potential contributions on large scales.

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