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Study of Redshifted HI from the Epoch of Reionization with Drift scan

Authors :
Paul, Sourabh
Sethi, Shiv K.
Subrahmanyan, Ravi
Shankar, N. Udaya
Dwarakanath, K. S.
Deshpande, Avinash A.
Bernardi, Gianni
Bowman, Judd D.
Briggs, Frank
Cappallo, Roger J.
Corey, Brian E.
Emrich, David
Gaensler, Bryan M.
Goeke, Robert F.
Greenhill, Lincoln J.
Hazelton, Bryna J.
Hewitt, Jacqueline N.
Johnston-Hollitt, Melanie
Kaplan, David L.
Kasper, Justin C.
Kratzenberg, Eric
Lonsdale, Colin J.
Lynch, Mervyn J.
McWhirter, S. Russell
Mitchell, Daniel A.
Morales, Miguel F.
Morgan, Edward H.
Oberoi, Divya
Ord, Stephen M.
Prabu, Thiagaraj
Rogers, Alan E. E.
Roshi, Anish A.
Srivani, K. S.
Tingay, Steven J.
Wayth, Randall B.
Waterson, Mark
Webster, Rachel L.
Whitney, Alan R.
Williams, Andrew J.
Williams, Christopher L.
Source :
2014 ApJ 793 28
Publication Year :
2014

Abstract

The detection of the Epoch of Reionization (EoR) in the redshifted 21-cm line is a challenging task. Here we formulate the detection of the EoR signal using the drift scan strategy. This method potentially has better instrumental stability as compared to the case where a single patch of sky is tracked. We demonstrate that the correlation time between measured visibilities could extend up to 1-2 hr for an interferometer array such as the Murchison Widefield Array (MWA), which has a wide primary beam. We estimate the EoR power based on cross-correlation of visibilities across time and show that the drift scan strategy is capable of the detection of the EoR signal with comparable/better signal-to-noise as compared to the tracking case. We also estimate the visibility correlation for a set of bright point sources and argue that the statistical inhomogeneity of bright point sources might allow their separation from the EoR signal.<br />Comment: 23 pages, 14 figures, accepted for publication in ApJ

Details

Database :
arXiv
Journal :
2014 ApJ 793 28
Publication Type :
Report
Accession number :
edsarx.1407.4620
Document Type :
Working Paper
Full Text :
https://doi.org/10.1088/0004-637X/793/1/28