Bayesian estimation of cross-coupling and reflection systematics in 21cm array visibility data

Geoff G. Murphy,Philip Bull,Mario G. Santos,Zara Abdurashidova, Tyrone Adams,James E. Aguirre,Paul Alexander,Zaki S. Ali, Rushelle Baartman,Yanga Balfour, Adam P. Beardsley,Gianni Bernardi,Tashalee Billings,Judd D. Bowman,Richard F. Bradley,Jacob Burba, Christopher Cain,Steven Carey,Chris L. Carilli,Carina Cheng,David R. DeBoer,Eloy de Lera Acedo,Matt Dexter, Joshua S. Dillon, Nico Eksteen,John Ely,Aaron Ewall-Wice,Nicolas Fagnoni,Randall Fritz,Steven R. Furlanetto,Kingsley Gale-Sides,Brian Glendenning,Deepthi Gorthi,Bradley Greig,Jasper Grobbelaar,Ziyaad Halday,Bryna J. Hazelton,Jacqueline N. Hewitt,Jack Hickish,Daniel C. Jacobs,Austin Julius,MacCalvin Kariseb, Nicholas S. Kern,Joshua Kerrigan,Piyanat Kittiwisit,Saul A. Kohn,Matthew Kolopanis,Adam Lanman,Paul La Plante,Adrian Liu, Anita Loots, David Harold Edward MacMahon,Lourence Malan, Cresshim Malgas, Keith Malgas, Bradley Marero, Zachary E. Martinot, Andrei Mesinger, Mathakane Molewa,Miguel F. Morales,Tshegofalang Mosiane, Steven G. Murray, Abraham R. Neben,Bojan Nikolic, Hans Nuwegeld,Aaron R. Parsons,Nipanjana Patra, Samantha Pieterse, Nima Razavi-Ghods,James Robnett, Kathryn Rosie, Peter Sims, Jackson Sipple, Craig Smith, Hilton Swarts, Nithyanandan Thyagarajan, Pieter van Wyngaarden, Peter K. G. Williams, Haoxuan Zheng

arxiv(2023)

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摘要
Observations with radio arrays that target the 21-cm signal originating from the early Universe suffer from a variety of systematic effects. An important class of these are reflections and spurious couplings between antennas. We apply a Hamiltonian Monte Carlo sampler to the modelling and mitigation of these systematics in simulated Hydrogen Epoch of Reionisation Array (HERA) data. This method allows us to form statistical uncertainty estimates for both our models and the recovered visibilities, which is an important ingredient in establishing robust upper limits on the Epoch of Reionisation (EoR) power spectrum. In cases where the noise is large compared to the EoR signal, this approach can constrain the systematics well enough to mitigate them down to the noise level for both systematics studied. Where the noise is smaller than the EoR, our modelling can mitigate the majority of the reflections with there being only a minor level of residual systematics, while cross-coupling sees essentially complete mitigation. Our approach performs similarly to existing filtering/fitting techniques used in the HERA pipeline, but with the added benefit of rigorously propagating uncertainties. In all cases it does not significantly attenuate the underlying signal.
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