2023
DOI: 10.1093/mnras/stac3439
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QUIJOTE scientific results – IV. A northern sky survey in intensity and polarization at 10–20 GHz with the multifrequency instrument

Abstract: We present QUIJOTE intensity and polarization maps in four frequency bands centred around 11, 13, 17, and 19 GHz, and covering approximately 29 000 deg2, including most of the northern sky region. These maps result from 9000 h of observations taken between May 2013 and June 2018 with the first QUIJOTE multifrequency instrument (MFI), and have angular resolutions of around 1°, and sensitivities in polarization within the range 35–40 µK per 1° beam, being a factor ∼2–4 worse in intensity. We discuss the data pro… Show more

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Cited by 32 publications
(47 citation statements)
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“…For this reason, an annulus around the sources is used, as mentioned at the beginning of this section. The lobes in the U map is an instrumental effect associated with intensity-to-polarization leakage due to the difference between the two co-polar beams, as explained in section 9.3 of Rubiño-Martín et al (2023). These are visible in this case because most of Crab polarized emission is contained in the Q direction in Galactic coordinates.…”
Section: Methodsmentioning
confidence: 81%
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“…For this reason, an annulus around the sources is used, as mentioned at the beginning of this section. The lobes in the U map is an instrumental effect associated with intensity-to-polarization leakage due to the difference between the two co-polar beams, as explained in section 9.3 of Rubiño-Martín et al (2023). These are visible in this case because most of Crab polarized emission is contained in the Q direction in Galactic coordinates.…”
Section: Methodsmentioning
confidence: 81%
“…In order to check the self-consistency of IFCAPOL, as well as have at hand an additional means of testing the stability of QUIJOTE data and the map-making algorithm (see Gómez-Reñasco et al 2012;Pérez-de-Taoro et al 2016;Rubiño-Martín et al 2023;Génova-Santos et al 2023), we have conducted a series of jackknife tests comparing the estimation of the main photometric and polarimetric quantities (I, P and 𝜙, but also Q and U individually) on two different maps, which have been produced by splitting the MFI wide survey data into two halves. The maps that we use are the so-called 'half-mission maps' and they are constructed by separating the individual observations (6 h each) according to the calendar date in each observing period (there are four in total, spread over 6 yr) and each telescope elevation (usually we have three or four observing elevations in each period).…”
Section: Internal Consistencymentioning
confidence: 99%
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