Search methods for UHECR anisotropies within the Pierre Auger Observatory Eric Armengaud (APC/IAP - Paris) for the Auger Collaboration March 2005 E. Armengaud - Moriond The Pierre Auger Observatory See talks by F. Arneodo and D. Newton Hybrid detection of UHECR (fluorescence + surface detectors) March 2005 Highest statistics with SD-only events Will be mostly used for anisotropy studies Still under construction (~700/1600 SD, 2/4 FD) E. Armengaud - Moriond Contents Angular reconstruction and resolution with the Surface Detector Exposure estimation methods Large-scale anisotropy search methods Source search methods March 2005 E. Armengaud - Moriond Angular reconstruction with SD Iterative fit with the arrival times of particles from the shower: Shower front ~ plane surface Global fit with LDF core location estimation If 4 tanks are hit : (variable) radius of curvature included Full Chi2 example : Weights σi : depend on clock discretization error (25 ns binning) distance to core (width of shower front increases with d) March 2005 E. Armengaud - Moriond Angular resolution with SD Estimation from simulations: Angular resolution ~ 1° Resolution improves with θ Resolution improves with E SD angular resolution can be derived from hybrid data Preliminary – Simulation Showers injected at 45o (Aires - SDSim) March 2005 E. Armengaud - Moriond Exposure estimation methods 1. 2. Need background estimation to analyse event maps Systematics can appear Poor statistics at the highest energies 2 strategies : Use our knowledge of detector acceptance Exposure derivation from the events (scrambling) March 2005 Preliminary raw event map (2004 subset : “T5 hexagons + Herald + >4tanks hit”) Equatorial coordinates – 3° smoothing E. Armengaud - Moriond Exposure derivation from the acceptance Auger exposure (> 4 tank events) Exposure in any direction (α,δ) is derived from integration of array acceptance over its working period Array growth and dead-times taken into account Zenith angle distribution: Analytically known when acceptance is saturated (high E) Derived from simulations or empirically fitted from the data at lower energies March 2005 E. Armengaud - Moriond Preliminary Exposure derivation : systematics Low-energy data, Jan-Feb period, Gal. coordinates Systematic effects, if correctly understood, can be taken into account in exposure computation Example : weather effects a(T,P) ~ 1 + α(T-To) + β(P-Po) [effects of shower physics, electronics, calibration...] T,P monitored at FD sites T captors on each SD station Correction to exposure for a given period is computed Day Night March 2005 E. Armengaud - Moriond Scrambling method From a given event set, construct N >>1 Monte-Carlo sets which conserve the original Zenith angle Θ distribution Azimuth φ distribution Solar time distribution Exposure = average of MC event maps Systematics, even uncontrolled, should be removed Real large-scale anisotropy patterns also removed!! Small statistical fluctuations remain March 2005 E. Armengaud - Moriond Simulation : Histogram of pixel relative values Scrambling Acceptance Large-scale feature analysis methods March 2005 E. Armengaud - Moriond Large-scale features : introduction Deflections by galactic fields : R/kpc ~(E/EeV)/ (Z B/μG) Large-scale patterns are expected in various scenarios: Low-energy, galactic sources High-energy sources in nearby structures Agasa detection at ~ 1 EeV : excess around GC Auger South looks directly towards the GC March 2005 Significance map (AGASA) at ~ 1EeV Possible ‘weather’ effect checked: - no signal in solar time harmonic analysis - signal in R.A. harmonic analysis E. Armengaud - Moriond From Rayleigh to dipole and Cℓ 1st harmonic analysis in R.A. : with and Dipole reconstruction (amplitude + orientation) – even with partial sky Higher Cℓ orders – even with partial sky : We develop the fluctuations of event number on spherical harmonic basis Assuming a stochastic and spectrally homogeneous field, we derive a Cℓ estimator: Due to partial sky coverage, we need to invert a mode-mixing matrix M(ℓ,ℓ’) to recover the ‘true’ Cℓ : Auger South exposure is large enough to do so. JCAP 0410 (2004) 008 March 2005 E. Armengaud - Moriond Angular power spectrum : example Low-energy data, Jan-May period, Gal. Coordinates, exposure subtracted Preliminary Small low-energy data sample (3 tanks only) Derived Cℓ : Raw exposure computation Weather systematics corrected Cℓ Multipole March 2005 E. Armengaud - Moriond Small-scale feature analysis methods March 2005 E. Armengaud - Moriond Source search : introduction Clusters found by Agasa at the highest energies Statistical significance still under debate; HiRes (stereo) does not confirm yet. Motivations : Directly pointing sources of UHECR Important constraints on extragalactic magnetic fields At lower E : neutrons from the GC (mean decay length @ 1 EeV ~ distance to GC) March 2005 E. Armengaud - Moriond Prescriptions on source searches Requirement : protect the Collaboration from wrong claims. A finite data set will always show some “pattern” if a large number of trials are made Method : a fixed excess probability P = 0.001 is distributed over a few a priori targets. Current ‘targets’: GC at low energy + Agasa/Sugar direction 3 nearby objects (Cen A, NGC0253, NGC3256) Targets can be changed in view of the data March 2005 E. Armengaud - Moriond Conclusions Auger angular resolution: ~ 1 degree improved for hybrid data Background estimation : scrambling Complementary methods (efficient tool to understand details of detector behavior) analytical computation Large scales : Rayleigh analysis Dipole reconstruction, angular power spectrum Small scales : Strict prescriptions to avoid wrong claims but blind source searches are also carried out to feed possible new prescriptions; Autocorrelation analysis, triangle area distribution... Analysis still going on: more events in the sky every day! March 2005 E. Armengaud - Moriond
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