# Detecting 21 cm EoR Signal using Drift Scans: Correlation of Time-ordered Visibilities

## TL;DR

This paper develops a formalism to analyze the coherence time of the 21 cm EoR signal in drift scans, identifying decorrelation timescales and foreground mitigation strategies using radio interferometer data.

## Contribution

It introduces a new formalism to determine the coherence timescale of the EoR HI signal in drift scans, accounting for physical decorrelation processes and foreground effects.

## Key findings

- HI signal decorrelation time scale is 2-20 minutes for relevant baselines
- Phase correlation can be stabilized, extending coherence time
- Point sources decorrelate faster than the HI signal, aiding foreground mitigation

## Abstract

We present a formalism to extract the EoR HI power spectrum for drift scans using radio interferometers. Our main aim is to determine the coherence time scale of time-ordered visibilities. We compute the two-point correlation function of the HI visibilities measured at different times to address this question. We determine, for a given baseline, the decorrelation of the amplitude and the phase of this complex function. Our analysis uses primary beams of four ongoing and future interferometers---PAPER, MWA, HERA, and SKA1-Low. We identify physical processes responsible for the decorrelation of the HI signal and isolate their impact by making suitable analytic approximations. The decorrelation time scale of the amplitude of the correlation function lies in the range of 2--20~minutes for baselines of interest for the extraction of the HI signal. The phase of the correlation function can be made small after scaling out an appropriate term, which also causes the coherence time scale of the phase to be longer than the amplitude of the correlation function. We find that our results are insensitive to the input HI power spectrum and therefore they are directly applicable to the analysis of the drift scan data. We also apply our formalism to a set of point sources and statistically homogeneous diffuse correlated foregrounds. We find that point sources decorrelate on a time scale much shorter than the HI signal. This provides a novel mechanism to partially mitigate the foregrounds in a drift scan.