A blind detection of a large, complex, Sunyaev–Zel’dovich structure^{†}^{†}thanks: We request that any reference to this paper cites ‘AMI Consortium:Shimwell et al. 2010’
Abstract
We present an interesting Sunyaev–Zel’dovich (SZ) detection in the first of the Arcminute Microkelvin Imager (AMI) ‘blind’, degreesquare fields to have been observed down to our target sensitivity of . In followup deep pointed observations the SZ effect is detected with a maximum peak decrement greater than 8 the thermal noise. No corresponding emission is visible in the ROSAT allsky Xray survey and no cluster is evident in the Palomar allsky optical survey. Compared with existing SZ images of distant clusters, the extent is large () and complex; our analysis favours a model containing two clusters rather than a single cluster. Our Bayesian analysis is currently limited to modelling each cluster with an ellipsoidal or spherical betamodel, which do not do justice to this decrement. Fitting an ellipsoid to the deeper candidate we find the following. (a) Assuming that the Evrard et al. (2002) approximation to Press & Schechter (1974) correctly gives the number density of clusters as a function of mass and redshift, then, in the search area, the formal Bayesian probability ratio of the AMI detection of this cluster is 7.9 :1; alternatively assuming Jenkins et al. (2001) as the true prior, the formal Bayesian probability ratio of detection is 2.1 :1. (b) The cluster mass is . (c) Abandoning a physical model with number density prior and instead simply modelling the SZ decrement using a phenomenological model of temperature decrement as a function of angular distance, we find a central SZ temperature decrement of K – this allows for CMB primary anisotropies, receiver noise and radio sources. We are unsure if the cluster system we observe is a merging system or two separate clusters.
keywords:
cosmology: observations – cosmic microwave background – galaxies:clusters – Sunyaev–Zel’dovich Astrophysics Group, Cavendish Laboratory, J J Thomson Avenue, Cambridge CB3 0HE
Owens Valley Radio Observatory, California Institute of Technology, Big Pine CA 93513
National Research Council Canada, Herzberg Institute of Astrophysics, Dominion Radio Astrophysical Observatory, P.O. Box 248, Penticton, BC, V2A 6J9, Canada
Departamento de Astrofísica, Universidad de La Laguna, E38205 La Laguna, Tenerife, Spain
Kavli Institute for Cosmology Cambridge, Madingley Road, Cambridge, CB3 0HA
School of Physics and Astronomy, Cardiff University, Cardiff, CF24 3AA
Hochschule Esslingen, Kanalstrae 33, Esslingen 73728, Germany
Joint ALMA Office, Av El Golf, 40, Piso 18, Santiago, Chile
University of Oxford, Denys Wilkinson Bldg, Keble Road, Oxford OX1 3RH
H. H. Wills Physics Laboratory, University of Bristol, Tyndall Ave, Bristol BS8 1TL
Kavli Institute for Particle Astrophysics and Cosmology, Physics Department, Stanford University, Stanford, CA, 94305, USA
Department of Astronomy, University of California at Berkeley, Berkeley, CA 94720
NRAO Technology Center, 1180 Boxwood Estate Road, Charlottesville, VA 22903, US
Dublin Institute for Advanced Studies, 31 Fitzwilliam Place, Dublin 2, Ireland
Columbia Astrophysics Laboratory, Columbia University, 550 West 120th Street, New York 10027, USA
1 Introduction
The Sunyaev–Zel’dovich (SZ) effect is the inverseCompton scattering of cosmic microwave background (CMB) photons from the hot plasma within clusters of galaxies (Sunyaev & Zel’dovich 1972, see e.g. Birkinshaw 1999 and Carlstrom, Holder & Reese 2002 for reviews). The surface brightness of an SZ signal does not depend on the redshift of the cluster and the integrated signal is only weakly dependent on via the angular diameter distance. Hence an SZeffect fluxdensitylimited survey can provide a complete catalogue of galaxy clusters above a limiting mass (see e.g. Bartlett & Silk 1994, Kneissl et al. 2001, Kosowsky 2003 and Ruhl et al. 2004).
Detecting and imaging the SZ effect has gradually become routine since it was first securely detected by Birkinshaw, Gull & Moffet (1981) and first imaged by Jones et al. (1993). Until recently, SZ observations have been directed almost entirely towards clusters selected optically or in Xray, for example with AMI (AMI Consortium: Zwart et al. 2010), AMiBA (Wu et al. 2008), APEX (Halverson et al. 2009), CBI (Udomprasert et al. 2004), CBI2 (Pearson et al. 2009), OCRA (Lancaster et al. 2007), OVRO/BIMA (Carlstrom, Joy & Grego 1996), RT (Grainge et al. 1996), SuZIE (Holzapfel et al. 1997), SZA (Muchovej et al. 2011) and the VSA (Lancaster et al. 2005). Now, however, SZ blind surveying is underway, with ACT and SPT having produced initial results (Hincks et al. 2010, Menanteau et al. 2010, Staniszewski et al. 2009, Vanderlinde et al. 2010 and High et al. 2010). The Arcminute Microkelvin Imager (AMI) is conducting a blind cluster survey at 16 GHz in twelve regions, each typically one deg, which contain no previously recorded clusters. The AMI cluster survey focuses on depth, aiming to detect weak SZeffect signals from clusters of galaxies with a mass above 2 , where corresponds to the total cluster mass within a spherical volume such that the mean interior density is 200 times the mean density of the Universe at the current epoch.
The outline of this paper is as follows. In Section 2, we give a brief description of the instrument, observations, data reduction and map making techniques. Identifying cluster candidates is described in Section 3 – we stress that some readers will wish to jump to the start of Section 3 which is an important overview of the three analysis methods and of their assumptions. We discuss how we apply a Bayesian analysis to the AMI data in Section 4 and present the results in Section 5.
We assume a concordance CDM cosmology, with = 0.3, = 0.7 and H = 70 km sMpc. The dimensionless Hubble parameter is defined as = H/(70 km sMpc). All coordinates are given at equinox J2000.
2 Instrument, observations, data reduction and mapping
2.1 The Arcminute Microkelvin Imager (AMI)
Sited at the Mullard Radio Astronomy Observatory, Cambridge ( above sea level), AMI consists of a pair of aperturesynthesis interferometric arrays optimised for SZeffect imaging centred at 16 GHz, with six frequency channels. The Large Array (LA) has a high resolution and fluxdensity sensitivity and is used primarily to detect contaminating sources which can then be subtracted from the Small Array (SA) maps. AMI is described in detail in AMI Consortium: Zwart et al. (2008) and the technical aspects of the arrays are summarised in Table 1. The SA has been operating since 2005 (see e.g. AMI Consortium: Barker et al. 2006, Scaife et al. 2008 and Scaife et al. 2009) and the LA since 2008 (see e.g. AMI Consortium: HurleyWalker et al. 2009). Pointed SZ observations have been straightforward but for blind observations we have felt it essential to get the best control of systematics that we can – for example, we found hardtounravel problems with LA pointing and errors in the electrical lengths of the lags in both the LA and the SA Fouriertransform correlators that produce small position shifts – we now have corrections for these problems that are adequate. We also have very good control over the influence of radio source contamination (see e.g. AMI Consortium: Franzen et al. 2009, Feroz et al. 2009, Waldram et al. 2010 and AMI Consortium: Davies et al. 2011).
SA  LA  
Antenna diameter  3.7 m  12.8 m 
Number of antennas  10  8 
Number of baselines  45  28 
Baseline length  5–20 m  18–110 m 
16GHz power primary beam FWHM  19.6  5.6 
Synthesized beam FWHM  3  30 
Array fluxdensity sensitivity  30 mJy  3 mJy 
Array brightness sensitivity  4.6 mK  16 mK 
Observing frequency  13.5–18.0 GHz  
Bandwidth  3.7 GHz  
Number of channels  6  
Channel bandwidth  0.75 GHz  
Polarization measured  I + Q 
2.2 Observations
The results presented here are from observations of field AMI002 which is centred on 02 59 30 +26 16 30. AMI002 is the first field to have been analysed as it was the first to reach a target depth of /beam. SA observations of AMI002 began on 2008 July 19 and ran until 2010 March 3, by which time 1200 hours of data had been gathered; LA observations began on 2008 August 8 and ran until 2010 January 10, collecting 630 hours of data. Using both the SA and the LA the field was typically observed for 8 hours in a day; this often comprised two individual observations each of 4 hours, split up with an observation of a fluxdensity calibrator. Observations were started at different positions in the field to improve the uv coverage.
A rastering technique was used for both the LA and the SA survey observations, where the pointing centres lie on a 2D hexagonallygridded lattice. The LA observations form a part of the 10C survey data, which are described in detail in AMI Consortium: Franzen et al. (2011). Additional dedicated pointings towards the cluster candidates are included to ensure that maximum sensitivity was obtained in the LA maps. For the 10C survey observations, the pointing centres are separated by 4 arcmin, which allows us to obtain close to uniform sensitivity over the field while minimising the observing time lost to slewing. In order to detect all important sources within the SA field, the LA field is slightly larger and the thermal noise is typically a factor of two lower than the SA thermal noise. To account for the SA map noise () increasing towards the edge of the field, the LA map consists of two distinct regions, the inner and the outer. The inner area of the LA field was observed to a noise level of , whereas the noise in the outer area was approximately twice as high. The outer region of the LA map is also used to detect bright sources lying just outside the SA field. The resulting LA noise map is shown in Figure 1. For the SA survey observations the pointing centres are separated by 13 arcmin giving a closetouniform noise level of over the map. The SA noise map is shown in Figure 2. Followup SA observations towards the cluster consisted of 50 hours of data centred at 03 00 08.66 +26 15 16.1 resulting in a noise level of 65.
The phase calibrator was observed for two minutes every hour using the SA and for two minutes every ten minutes using the LA. The phase calibrator used for both the LA and the SA observations was J0237+2848. The amplitude calibration for the SA uses 3C286 and 3C48 which are observed daily; the assumed flux densities are shown in Table 2 (AMI Consortium: Franzen et al. 2011). The LA was fluxdensitycalibrated from the SA measurements of J0237+2848; we have adopted this approach to minimise interarray calibration errors. Although the flux density of J0237+2848 is known to vary at AMI frequencies, with a mean variability index of 3.1 over 269 days (AMI Consortium: Franzen et al. 2009), we ensured that SA measurements of this source were always within 30 days of the LA observations. This calibration scheme is described in detail in AMI Consortium: Franzen et al. (2011) and provides fluxdensity calibration errors of less than 5%.
Channel  

3C48  3C286  
1  14.2  1.850  3.663 
2  15.0  1.749  3.535 
3  15.7  1.658  3.414 
4  16.4  1.575  3.308 
5  17.1  1.500  3.206 
6  17.9  1.431  3.111 
2.3 Data Reduction
There are 65 LA observations and 337 SA observations of AMI002, each being passed through reduce, the inhouse software developed for the VSA and AMI data reduction. reduce was used to flag telescope pointing errors, shadowing effects and hardware errors. The data are also flagged for interference before being Fourier transformed into the frequency domain, where they are corrected for systemtemperature variations, phasecalibrated and amplitudecalibrated. In the frequency domain the data are again searched for interference and baselines with inconsistent fluxdensity values are flagged. The data are reweighted so that baselines and channels with the lowest noise have the highest weight. The data are then stored as uvfits files, with each raster pointing being treated as an independent source within the fits definition. This reduction scheme follows that of AMI Consortium: Davies et al. (2009). Individual uvfits files for the LA and the SA are combined into a single multisource uvfits file for each array, which are taken into aips ^{1}^{1}1http://www.aips.nrao.edu for imaging.
The SA data were checked for systematics using two jackknife tests. In test (a), calibrated visibilities from “plus” correlator boards are subtracted from those obtained from “minus” correlator boards – the signal is the same for both correlations but the latter inserts an additional 180 phase shift into the signal from one antenna (see Holler et al. 2007 for a full description of the AMI correlator). For test (b), data obtained before the weighted median date of the visibilities are subtracted from data obtained afterwards. Either test will remove signals present in both halves of the data but noise or systematics that vary with time will remain. For the followup pointed SA observations presented in this paper test (a) revealed no systematics and test (b) showed a negative feature with a fluxdensity of 0.35mJy/beam associated with the 2.26mJy/beam source at 03:00:29.46 +26:18:39.9. Investigation demonstrated that this residual was a consequence of the fluxdensity of the source being dependent upon the elongation of the synthesized beam. For reasons of scheduling, it became clear that the synthesized beam from the first half of data was elongated in the NWSE direction and the source was measured to have a fluxdensity of 2.51mJy/beam. In the second half of the data the synthesized beam was extended in the NESW direction and the measured fluxdensity was 2.03mJy/beam. Maps of the jackknifed pointed SA observations are shown in Figure 3.
2.4 LA mapmaking and sourcefinding
LA maps for each AMI channel and the continuum were produced for each of the pointings within the AMI002 field using the aips task imagr. The maps are cleaned to three times the map thermalnoise without any individual clean boxes. The individual pointings are combined using the flatn task, discarding data lying outside the 10% point of the power primary beam. flatn is also used to create appropriatelyweighted noise maps using the thermal noise levels in the individual pointings.
Source finding is carried out using the LA continuum map with the AMI sourcefind software. All pixels on the map with a flux density greater than , where is the noise map value for that pixel, are identified as peaks. The flux densities and positions of the peaks are determined using a tabulated Gaussian sinc degridding function to interpolate between the pixels. Only peaks where the interpolated flux density is greater than are identified as sources. The aips routine jmfit fits a twodimensional Gaussian to each source to give the angular size and the integrated flux density for the source. These fitted values are compared to the pointsource response function of the telescope to determine whether the source is extended on the LA map. The mapping and the source finding techniques are described in more detail in AMI Consortium: Franzen et al. (2011).
For each source we use the sourcefind algorithm to find the flux densities in the individual AMI LA channel maps at the positions of the detected sources. By assuming a powerlaw relationship between flux density and frequency () we use the channel fluxdensities to determine the spectral index for each source. The spectral index is calculated using an MCMC method based on that of Hobson & Baldwin (2004) – the prior on the spectral index has a Gaussian distribution with a mean of 0.5 and of 2.0, truncated at . The minimum spectral index of a source in the AMI002 field was found to be 0.0 and the maximum was 1.8. The map noise in each channel map at the position of the source was used to calculate the weighted mean of the channel frequencies and determine the effective central frequency of the source. The effective central frequency varies between pointings due to flagging applied in reduce. Unlike in AMI Consortium: Franzen et al. (2011), the data are not reweighted to the same frequency because this leads to a small loss of sensitivity.
In total we detect 203 sources in the AMI002 LA map at four times the LA map noise (), 11 of which are extended. The most extended source has an area of 1.9 LA synthesized beams. As the SA synthesized beam is significantly larger we do not expect any extended sources in the SA map. For each source we catalogue the rightascension , declination , flux density at the central frequency , spectral index and the central frequency. If a source is extended we use the centroid of the fitted Gaussian as the position and the integrated flux density instead of the peak flux density.
3 Identifying and modelling cluster candidates
Our analysis necessarily depends in part on the fact that we do not know – in the absence of e.g. optical spectroscopic observations – the redshift of the blind SZ clusters. We have thus carried out our analysis in two main ways, both fully Bayesian and based on Hobson & Maisinger 2002, Marshall et al. 2003 and Feroz et al. 2009, as follows.
(1) Physical model. We assume an isothermal profile for the gas density as a function of radius; we assume all the cluster kinetic energy is in the internal energy of the cluster gas and that the relation between gas temperature and total cluster mass is then given by the virial theorem; and we assume the prior probability for the comoving number density of clusters as a function of total mass and redshift is given by previous theoretical/simulation work – we here use the predictions of Evrard et al. (2002) and Jenkins et al. (2001) and note that more recent such work does not make a substantial difference for our purposes. With these assumptions we are then able to (a) estimate the significance of an SZ detection, and (b) produce probability distributions of physical cluster parameters such as mass and radius. For both (a) and (b) the methodology takes into account radio sources, receiver noise, and the statistical properties of the primordial CMB structure; it cannot take into account other effects that have not been dealt with in, for example, telescope design, telescope commissioning, observing and data reduction.
(2) Phenomenological model. Some or all of the assumptions in (1) may be poor or wholly wrong. Accordingly in (2), we make far fewer assumptions. We assume isothermality and that the temperature decrement as a function of angular distance is given by a model. This model cannot give probability distributions of values of physical importance such as mass, but still does give the significance of the SZ detection in the presence of radio sources, receiver noise and primordial CMB structure; like (1) it cannot take into account other effects that have not previously been dealt with.
We give the significance of decrement detection in a third way, the decrement signal in units of receiver noise. We point out that for AMI this method of course takes no account of primordial CMB structures but does take into account radio sources, and the higher fluxdensity sources have had their SA fluxdensities estimated in a Bayesian way from SA data and priors from LA measurements – this allows for interarray calibration problems and for LA and SA observations that were not precisely simultaneous. Again, like (1) and (2), this method cannot take into account other effects that have not previously been dealt with.
3.1 Physical model
Our primary Bayesian analysis is based on a physical model for the cluster producing the SZ effect. The SA observations of the AMI002 survey field are analysed using a model characterised by the parameters , where are cluster parameters and are source parameters (Feroz et al. 2009). Here and give the cluster position, is the orientation angle measured from N through E, is the ratio of the lengths of the semiminor to semimajor axes, describes the cluster gas density according to Cavaliere & FuscoFemiano (1976,1978), where the gas density decreases with radius
(1) 
is the core radius, is the cluster total mass within a radius and is the cluster redshift. is defined as the radius inside which the mean total density is 200 times the critical density . Feroz et al. (2009) and AMI Consortium: RodríguezGonzálvez et al. (2011) describe the parameters and the methods used to extract these from the data in more detail. For this work we sample from , , ,, , , and and derive other cluster parameters such as the cluster gas mass and the cluster temperature . We also assume a masstemperature relationship characteristic of a virialised cluster; this is the favoured model (M3) in AMI Consortium: RodríguezGonzálvez et al. (2011), although we sample from rather than , see also AMI Consortium: Olamaie et al. 2010. The total cluster mass within is
(2) 
The gas fraction is derived from the results of Komatsu et al. (2010) taking into account our value for and that the gasmass fraction is of the baryonic mass fraction. The ellipticity of the clusters is calculated by applying a coordinate transformation from point () on the sky:
(3) 
Lines of constant represent ellipses enclosing an area , where is the semiminor axis and is the semimajor axis. This transforms the circular slices perpendicular to the line of sight to an ellipse, keeping the area of the ellipse the same as the circular slice. A summary of the priors used on the model parameters is shown in Table 3.
Parameter  Prior 

Source position ()  A deltafunction prior using the LA positions 
Source flux density ()  A Gaussian centred on the LA continuum value with a of 40% 
Source spectral index ()  A Gaussian centred on the value calculated from the LA channel maps with the LA error as 
Redshift ()  Joint prior with between 0.2 and 2.0 (Jenkins et al. 2001 or Evrard et al. 2002) 
Core radius ()  Uniform between 10 and 1000 
Beta ()  Uniform between 0.3 and 2.5 
Mass ()  Joint prior with between 2.0 and 5 (Jenkins et al. 2001 or Evrard et al. 2002) 
Gas fraction ()  Deltafunction prior at 0.11 (Komatsu et al. 2010) 
Cluster Position ()  Uniform search triangle (Figure 4) 
Orientation angle ()  Uniform between 0 and 180 
Ratio of the length of semiminor to semimajor axes ()  Uniform between 0.5 and 1.0 
The above approach has already been used to detect the SZ effect from AMI observations of known clusters in AMI Consortium: Zwart et al. (2010) and AMI Consortium: RodríguezGonzálvez et al. (2011). However, for blind cluster surveys we are faced with the additional problem that we do not have a priori evidence for a cluster at a particular position (or redshift). In analysing a survey field, the marginalised posterior distribution in the plane will typically contain a number of local peaks; some of these may correspond to the presence of a real cluster, whereas others may result from chance statistical fluctuations in the primordial CMB and/or instrument noise. Each local peak in the posterior is automatically identified by the MultiNest sampler (Feroz & Hobson 2008 and Feroz, Hobson & Bridges 2008) used in our Bayesian analysis, and may subsequently be analysed independently to obtain cluster parameter estimates.
To determine the significance of each such putative cluster detection, we perform a Bayesian model selection, which makes use of estimated cluster number counts from analytical theory (e.g. the Evrard et al. 2002 approximation to Press & Schechter 1974) and numerical modelling (e.g. Jenkins et al. 2001) together with measurements of the rms mass fluctuation amplitude on scales of size 8 Mpc at the current epoch (see e.g. Lahav et al. 2002, Seljak et al. 2005 and Vikhlinin et al. 2009). It must be borne in mind, however, that the actual values of the number density of clusters, particularly at high redshift, are uncertain and hence the degree of applicability of these as priors is unclear.
In our Bayesian model selection, we calculate the formal Bayesian probability of two hypotheses: the first, , assumes at least one cluster with is associated with the local peak in the posterior distribution under consideration; the second, , assumes no such cluster is present. Here is the limiting cluster mass that can be detected and is the maximum mass of a cluster. In particular, we consider the ratio (also known as the Bayes factor, or the odds) of these two formal probabilities
(4) 
To evaluate this ratio, let us first denote by the area in the plane of the ‘footprint’ of the local posterior peak under consideration (we will see below that a precise value for is not required). Also, we denote by the hypothesis that there are clusters with with centres lying in the footprint , so that
(5) 
Thus equation (4) can be written as
(6) 
where we have used Bayes’ theorem in the second equality. Assuming that objects are randomly distributed over the sky, then
(7) 
where is the expected number of clusters with in a region . This is given by , where is the expected number of clusters per unit sky area:
(8) 
where is the comoving number density of clusters as a function of redshift and mass. For the calculation of , we follow the method of either Evrard et al. (2002) or Jenkins et al. (2001). If we further assume that there is very low probability of two or more clusters having their centres in the region () we can neglect and larger powers of , so that equation (6) can be approximated simply by
(9) 
where the is the ‘local evidence’ (see Feroz et al. 2009) associated with the posterior peak under consideration in the singlecluster model, and is the ‘null’evidence (which does not depend on ).
Our Bayesian analysis uses MultiNest to calculate the Bayesian evidence for the different hypotheses (Feroz & Hobson 2008 and Feroz, Hobson & Bridges 2008). When searching for clusters in some survey area , however, a uniform prior is assumed on the position of any cluster, rather than assuming a uniform prior over the footprint . Thus, MultiNest returns a local evidence associated with the posterior peak that is given by
(10) 
and the ‘null’ evidence remains unchanged. Thus, if we denote the expected number of clusters in the survey area by , then (6) becomes
(11) 
Here and are outputs of MultiNest and is easily calculated from (8) given some assumed cluster mass function, and so may then be calculated. In our analysis and the value that we calculate is smaller than that obtained by setting the prior ratio equal to unity. Jeffreys (1961) provides an interpretive scale for the value, as do revised scales such as Gordon & Trotta (2007). Moreover, the value in (11) can be turned into a formal Bayesian probability that the putative detection is indeed due to a cluster with mass and centre lying in , which is given by
(12) 
3.2 Phenomenological model
An alternative approach is to set aside the physical cluster model and instead adopt a model based on a phenomenological description of the SZ decrement itself.
In this case, at the location of each putative cluster detection identified using the physical cluster model, we simply fit a profile to the SZ temperature decrement using the parameters , and to characterise shape and magnitude of the decrement according to
(13) 
The assumed priors on these parameters are summarised in Table 4.
Parameter  Prior 

Uniform between  
Uniform between 20 and 500  
Uniform between 0.4 and 2.5 
In this analysis we continue to use Gaussian priors on the flux densities and on the spectral indices of significant sources, and deltafunction priors for faint sources. We also assume a Gaussian prior () on position centred on each decrement.
This approach allows us to produce a posterior distribution that directly describes the temperature decrement and also allows us to evaluate what proportion of the decrement is caused by the SZ effect, while also accurately accounting for point sources, receiver noise and the statistical properties of the primary CMB anisotropy.
4 The analysis
The AMI002 SA survey map contains 24 individual pointing centres. A single Bayesian analysis of the entire field is prohibitively computationally expensive because of the large quantity of data and the high dimensionality of the parameter space. Instead three pointings are analysed at a time. Each set of three pointing centres form a triangle and in total there are 30 different triangles in the AMI002 field, an example of which is shown in Figure 4.
To reduce the dimensionality of the parameter space further, all sources located at positions where the primary beam has fallen below 10 of its maximum, together with sources that have a flux density measured on the LA that is lower than , are given deltafunction priors on their positions, spectral indices and flux densities. We search for clusters in a triangular area which is an enlarged version of the triangle formed between the pointing centres – the radius of the inscribed circle is 3 larger. This allows us to detect clusters out to the edge of our most sensitive areas and ensures that the search areas belonging to adjacent triangles overlap. The minimum rms noise within a search triangle in the AMI002 field is and the maximum is . The limiting cluster total mass is set to and the maximum cluster mass to . The limiting mass is conservative given the radio fluxdensity sensitivity of our observations.
We follow up our most significant detections with pointed observations towards the candidate. The data from these observations can be analysed with our Bayesian method with lower dimensionality because there are fewer sources within 0.1 of the power primary beam with flux densities greater than . For the followup pointed observations the prior on the cluster position is altered to a 1000 x 1000 box centred on the pointing centre and we allow our Bayesian analysis software to fit the source positions with a Gaussian prior centred on the LA position with an error of 5.
5 Results and Discussion
The most significant candidate cluster detection made using the Bayesian analysis of the AMI SA survey field AMI002 is located at J 03 00 16.5 +26 13 59.5, where MultiNest identifies a single marginalised posterior peak in the plane centred on this location. The significance of the cluster detection is when we use Model (1) and the Evrard et al. (2002) prior and when we apply Model (1) using the Jenkins et al. (2001) prior. The relevant area of the survey field is shown in Figure 5 before and after source subtraction (see below). In the search triangle that contains our cluster candidate there are 59 sources within 0.1 of the power primary beam, 43 of which have a flux density below ; the other 16 have been modelled with our Bayesian analysis. The location of the marginalised posterior peak is indicated by the small box in the figures.
At this position in our survey field is a highlyextended, noncircular negative feature with a peak fluxdensity decrement of 0.6 mJy (). SA observations are mapped in aips using the same method as for the LA, but with a pixel size of . We subtract sources from the uvfits data using the inhouse software muesli. muesli performs the same function as the aips task uvsub; however, it is optimised for processing AMI data. The parameters of the 16 modelled sources are shown in Table 5; we find no evidence that any of them is extended relative to the LA synthesised beam. The source subtraction leaves very little residual flux density on the map, indicating that the phase stability and calibration of AMI is robust. The most significant sourcesubtraction residuals are towards the edge of the SA power primary beam where we expect the phase errors to be larger and the beam model to be less accurate.
Right ascension  Declination  Flux density  Spectral index  Mean frequency  Flux density 

(J2000)  (J2000)  (mJy)  ( GHz)  
03:00:24.53  +26:19:40.83  1.21 0.12  +1.38 0.38  15.63  
03:00:29.46  +26:18:39.95  2.26 0.12  +0.71 0.29  15.64  
02:59:06.92  +26:15:29.59  0.26 0.09  +1.46 1.10  15.57  
02:59:50.35  +26:25:22.37  0.23 0.11  +0.51 1.24  15.58  
02:59:39.76  +26:05:56.15  0.40 0.09  +2.31 1.06  15.52  
03:00:15.23  +26:19:25.56  1.44 0.11  +1.59 0.40  15.64  
02:59:23.57  +26:05:54.53  0.40 0.10  +0.81 1.24  15.54  
02:59:55.16  +26:27:26.24  8.49 0.22  +0.33 0.07  15.59  
02:59:10.71  +25:54:31.60  3.81 0.41  +1.05 0.16  15.57  
02:59:35.43  +26:17:26.77  0.64 0.09  0.22 0.94  15.53  
03:00:49.28  +26:15:05.70  0.53 0.12  +0.40 0.42  15.67  
02:59:29.68  +26:09:46.99  0.50 0.07  +1.71 1.26  15.55  
02:59:41.05  +26:02:20.41  1.58 0.12  +1.36 0.36  15.54  
02:59:57.17  +25:53:56.17  1.40 0.23  +2.20 0.34  15.58  
03:00:01.33  +26:21:01.55  1.96 0.12  0.45 0.31  15.56  
02:58:25.32  +26:16:59.59  1.63 0.33  +0.95 0.27  15.58 
The cluster candidate was followed up with a pointed observation. Within the 10% point of the SA power primary beam 31 sources were observed with the LA, 9 of which were detected at above 4 and are modelled by our Bayesian analysis. These 9 sources are a subset of the 16 sources modelled on the Bayesian analysis of the survey data; they are indicated by a ‘tick’ in the last column of Table 5. We find no evidence that any of these 9 sources is extended relative to the LA synthesised beam. The image produced from the pointedobservation data is shown before and after source subtraction in Figure 6. Again we see a highlyextended, noncircular negative feature with a peak fluxdensity decrement of 0.6 mJy (). The SA synthesized beam and the uv coverage for the followup pointed observation is shown in Figure 7. To estimate the maximum level of contamination from the residuals of the sources in Table 5, we assume that the residual is equal to the error in the source flux and sum the absolute value of the synthesized beam contribution from each of these residuals at the positions of candidate 1 and candidate 2, we find contributions of 32 and 70 respectively. Hence, if in the unlikely case all sources leave a feature of magnitude equal to the error in that source flux, and that these features conspire in such a way to contribute only negative flux at the positions of candidates 1 and 2, we find the contribution to the total SZ signal is minimal. This calculation does not account for any errors in the shape of the synthesized beam, due to e.g. antenna positions.
Our Bayesian analysis of the pointedobservation data, which have a higher signaltonoise ratio than the survey data, finds two local peaks in the marginalised posterior distribution in the plane. These cluster candidates are: candidate 1 at J 03 00 14.8 +26 10 02.6 and candidate 2 at J 03 00 08.9 +26 16 29.1. The Model (1) significance of the two cluster detections are and respectively when we apply the Evrard et al. (2002) model and and respectively when we apply the Jenkins et al. (2001) model. These larger values for the ratio, as compared with those obtained using the survey data, result from the higher signaltonoise ratio of the pointed observation. The evidence values, ratios and related parameters for the survey observations and the pointed observation are summarised in Table 6. We also made a direct comparison of the Bayesian evidence for a model containing two clusters and a model containing just a single cluster and find that the Bayesian evidence is 7.6 higher for the model containing two clusters.
Parameter  Survey  Pointed (candidate 1)  Pointed (candidate 2) 

Search area (steradians)  2.00  2.35  2.35 
log()  56351.1  29692.1  29687.3 
log()  56350.9  29692.0  29687.1 
log()  56346.6  29678.8  29678.8 
0.11  0.14  0.14  
0.29  0.34  0.34  
8.7  7.9  560  
26  2.1  1800 
The 1D and 2D marginal posterior distributions for a selection of the physical parameters of each cluster are shown in Figure 8. We are able to constrain , even though it is dengenerate with . As is large this degeneracy causes the derived value to be low. We are able to constrain the well known degeneracy between and and find that values of 1.0 do not fit our data. We also find that the bestfit ratio of the lengths of the semiminor to semimajor axes is 0.6 and 0.75 respectively; the orientation angles are 122 and 78.
Finally, we used Model (2) and performed a Bayesian analysis where we simply fit a profile to the SZ temperature decrement directly. The 1D and 2D marginal posterior distributions for the parameters , and are shown in Figure 9. From our data we are able to tightly constrain at , but we are unable to accurately derive . The mean values and 68% confidence limits for each parameter are given in Table 7 and demonstrate significance of the detections directly.
Parameter  Pointed (candidate 1)  Pointed (candidate 2) 

We have looked for optical identification of the cluster in the Palomar allsky survey and Xray identification from ROSAT ^{2}^{2}2We have made use of the ROSAT Data Archive of the MaxPlanckInstitut fr extraterrestrische Physik (MPE) at Garching, Germany. – no cluster identification is evident. We plan to perform Xray and optical followup observations.
6 Conclusions

We have presented a large, complex Sunyaev–Zel’dovich structure in an AMI blind field. The structure may be two separate components or be a single merging system.

A Bayesian analysis using a physical model for the cluster (including assumed priors on the number density of clusters) was used to constrain cluster parameters such as and . Using the Bayesian evidences we have calculated formal probabilities of detection taking into account point sources, receiver noise and the statistical properties of the primary CMB anisotropy. For the deeper component we find a formal probability of detection ratio of 7.9 :1 when assuming the Evrard et al. (2002) cluster number count and 2.1 :1 when assuming Jenkins et al. (2001) as the true prior. We derive a cluster mass of .

A Bayesian analysis using a phenomenological model of the gas distribution was also used to quantify the significance of the detection and again taking into account point sources, receiver noise and the statistical properties of the primary CMB anisotropy. For the deeper component we find .

In our pointed followup observation the cluster system is detected with a high significance, with each map indicating that there is a 0.6mJy/beam peak decrement () towards the deeper component and an integrated decrement flux density () of . The other component has a 0.5mJy peak decrement and an integrated decrement of 0.7mJy.

Using the approximation we anticipate that the AMI blind cluster survey will detect clusters with at .
7 Acknowledgments
We thank the anonymous referee for providing us with very constructive comments and suggestions. We thank PPARC/STFC for support of AMI and its operations. We are grateful to the staff of the Cavendish Laboratory and the Mullard Radio Astronomy Observatory for the maintenance and operation of AMI. CRG, MLD, MO, MPS, TMOF and TWS acknowledge PPARC/STFC studentships. This work was performed using the Darwin Supercomputer of the University of Cambridge High Performance Computing Service (http://www.hpc.cam.ac.uk/), provided by Dell Inc. using Strategic Research Infrastructure Funding from the Higher Education Funding Council for England, and the Altix 3700 supercomputer at DAMTP, University of Cambridge supported by HEFCE and STFC. We are grateful to Stuart Rankin and Andrey Kaliazin for their computing assistance.
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