The Anisotropy of the Microwave Background to l = 3500: Deep Field Observations with the Cosmic Background Imager
B. S. Mason, T. J. Pearson, A. C. S. Readhead, M. C. Shepherd, J. L. Sievers, P. S. Udomprasert, J. K. Cartwright, A. J. Farmer, S. Padin, S. T. Myers, J. R. Bond, C. R. Contaldi, U. -L. Pen, S. Prunet, D. Pogosyan, J. E. Carlstrom, J. Kovac, E. M. Leitch, C. Pryke, N. W. Halverson, W. L. Holzapfel, P. Altamirano, L. Bronfman, S. Casassus, J. May, M. Joy
TL;DR
The paper reports deep-field measurements of the cosmic microwave background anisotropy with the Cosmic Background Imager, extending the measured spectrum to ell up to 3500. It confirms the damping of primary anisotropies and maps the tail of the spectrum out to ell ~ 2000, while finding a significant excess power at ell > 2000 that exceeds standard intrinsic models. The analysis employs a robust maximum-likelihood framework with careful subtraction of discrete radio sources, complemented by OVRO 31 GHz source measurements and NVSS-based statistics to control foregrounds. The authors discuss possible origins for the high-ℓ excess, including secondary Sunyaev-Zeldovich anisotropy, and emphasize the need for further observations to pinpoint its origin and implications for sigma_8 and structure formation.
Abstract
We report measurements of anisotropy in the cosmic microwave background radiation over the multipole range l ~ 200 - 3500 with the Cosmic Background Imager based on deep observations of three fields. These results confirm the drop in power with increasing l first reported in earlier measurements with this instrument, and extend the observations of this decline in power out to l \~ 2000. The decline in power is consistent with the predicted damping of primary anisotropies. At larger multipoles, l = 2000 - 3500, the power is 3.1 sigma greater than standard models for intrinsic microwave background anisotropy in this multipole range, and 3.5 sigma greater than zero. This excess power is not consistent with expected levels of residual radio source contamination but, for sigma_8 >~ 1, is consistent with predicted levels due to a secondary Sunyaev-Zeldovich anisotropy. Further observations are necessary to confirm the level of this excess and, if confirmed, determine its origin.
