ETmiss Performance in ATLAS data 2010

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Presentation transcript:

ETmiss Performance in ATLAS data 2010 Rosa Simoniello Università degli Studi di Milano & INFN

Italian groups working on ETmiss Milano group (Donatella Cavalli, Silvia Resconi, Caterina Pizio, Rosa Simoniello): Developed the ETmiss algorithm  Collaboration with: Peter Lock (Arizona), Adam Yurkewicz (Stony Brook) MissingET package maintenance Silvia Resconi co-convener of “JetEtmiss data preparation Task Force” Strongly involved in ETmiss commissioning since first data taking (co-editors of all ETmiss CONF notes in ATLAS) Frascati group (Mario Antonelli, Marianna Testa): Developed energy flow calibration for the low energy contribution to the ETmiss Determination of the ETmiss absolute scale using W ℓn events (taking over from Caterina Pizio) V ATLAS ITALIA - Rosa Simoniello

ETmiss CONF notes Note: ATLAS-COM-CONF-2010-008 Title: Performance of the missing transverse energy reconstruction in minimum bias events at a Center-of-Mass Energy of 900 GeV and 2.36 TeV with the ATLAS detector (15 Feb 2010) Editors: Cavalli, D.; Pralavorio, P. Note: ATLAS-COM-CONF-2010-039 Title: Performance of the missing transverse energy reconstruction in proton-proton collisions at center-of-mass energy of 7 TeV with the ATLAS detector (12 May 2010) Editors: Baak, M.; Resconi, S. Note: ATLAS-COM-CONF-2010-059 Title: Performance of the Missing Transverse Energy Reconstruction and Calibration in Proton-Proton Collisions at a Center-of-Mass Energy of 7 TeV with the ATLAS Detector (15 Jun 2010) Editors: Cavalli, D.; Liang, Z.; Yurkewicz, A. Note: ATLAS-COM-CONF-2011-035 Title: Reconstruction and Calibration of Missing Transverse Energy and Performance in Z and W events in ATLAS Proton-Proton Collisions at √s=7 TeV (approved 17 May 2011) Editors: Cavalli, D.; Dobson, E. V ATLAS ITALIA - Rosa Simoniello

Towards the ETmiss PAPER All ETmiss results will enter in the ETmiss PAPER (PERF-2011-007) (D. Cavalli, S. Resconi co-editors) that should be published in June. Supporting note: Note: ATL-COM-PHYS-2011-417 Title: Reconstruction and Calibration of Missing Transverse Energy and Performance in Z and W events in ATLAS Proton-Proton Collisions at √s=7 TeV (supporting the respective CONF note) Authors: 16  Italians: Antonelli, M.; Cavalli, D.; Pizio, C.; Resconi, S.; Simoniello, R., Testa, M. Note: ATL-COM-PHYS-2011-496 Title: Performance of Missing Transverse Energy Reconstruction and Calibration in QCD and minimum bias events in ATLAS Proton-Proton Collisions at √s=7TeV Authors: 5  Italians: Cavalli, D.; Resconi, S.; Simoniello, R. Note: ATL-COM-PHYS-2011-495 Title: Determination of the absolute scale of the Missing Transverse Energy using W ℓn events selected by ATLAS in Proton-Proton Collisions at √s=7 TeV Authors: 4  Italians: Antonelli, M., Pizio; C.; Testa, M. V ATLAS ITALIA - Rosa Simoniello

Outline General information about ETmiss reconstruction RefFinal algorithm Performance in events with different topologies fmiss and ∑ET distributions ETmiss Systematic Uncertainty ETmiss scale V ATLAS ITALIA - Rosa Simoniello

ETmiss reconstruction in ATLAS ETmiss is a complex event quantity: It’s calculated adding all significant signals from all detectors: Calorimeters signals (input: cells, TopoClusters) Muon signals Tracks in region where the Calorimeter and the Muon Spectrometer are inefficient V ATLAS ITALIA - Rosa Simoniello Missing Transverse Energy: { Sum of energy of all particles seen in the detector

ETmiss importance in ATLAS physics TRUE ETMISS FAKE ETMISS True ETmiss is due to not interacting particles in the detectors (n, LSP) A good ETmiss measurements is crucial for studies of many physics channels in ATLAS: W  ln, Ztt, ttbar SM Higgs (VBFhtt, tthtt) MSSM Higgs (A/Htt, H±tn)  reconstruct the invariant tt mass SUSY (R-parity conservation) large ETmiss signature  LPS Particles outside the detector acceptance Other particles arriving at the detector Energy lost in dead materials Electronic noise Pileup Problems in the detectors A bad measurements of ETmiss could fake a non-zero reconstructed Etmiss in the event with no physical ETmiss  QCD with fake ETmiss are a background for inclusive no-lepton SUSY events V ATLAS ITALIA - Rosa Simoniello

RefFinal algorithm RefFinal algorithm Best configuration V ATLAS ITALIA - Rosa Simoniello RefFinal algorithm Best configuration Eflow algorithm RefFinal algorithm

RefFinal Algorithm MET_RefEle MET_Ref MET_RefTau MET_RefJet MET_SoftJet MET_RefMuon MET_Muon + = Go back to constituent Calorimeter Topoclusters  Cells → apply overlap removal at Cell level → Cell calibration weights dependent on the object → add them to calculate partial terms Electrons Jets Muons TopoClusters not in objects Taus Photons SoftJets MET_CellOut MET_RefFinal V ATLAS ITALIA - Rosa Simoniello cells are calibrated on the basis of the reconstructed physics object to which they belong Very flexible algorithm  it allows to use the best calibration for each object

RefFinal Configuration This configuration gives the best performance (see CONF note) Recently recommended for future analysis in ATLAS It is based on LCW (Local Hadron) calibration Calibration of topoclusters outside reconstructed objects improved adding tracks information  next slide V ATLAS ITALIA - Rosa Simoniello

Eflow Algorithm for CellOut V ATLAS ITALIA - Rosa Simoniello The CellOut term is improved using reconstructed tracks: add tracks which do not reach the calorimeter or do not seed a topocluster when a track is associated to a topocuster the track momentum is used instead of the topocluster energy.

Etmiss performance in W/Z/Dijets events V ATLAS ITALIA - Rosa Simoniello ETmiss distributions fmiss distributions Diagnostic plot Resolution curves Linearity ∑ET distribution Etmiss performance in W/Z/Dijets events

Data and MC samples Analyzed data 2010: Zll, Wln: Dijets: Minbias: ≈ 36pb-1 similar selections used by WZ group Dijets: ≈ 600nb-1 (prescaled trigger) 2 jets with pT>25GeV Minbias: ≈ 0.3nb-1  period A V ATLAS ITALIA - Rosa Simoniello Monte Carlo: Pythia/MC@NLO samples (Zll, Wln, Jx, minbias, EW backgrounds) Same selection applied for data In-time pileup

ETmiss distribution Zee Zµµ Wen Wµn ATLAS Preliminary ATLAS Preliminary Wen Wµn ATLAS Preliminary ATLAS Preliminary V ATLAS ITALIA - Rosa Simoniello MC normalised to data, after each MC sample is weighted with its cross-section and reweighted to the data nVertex distribution Good data-MC agreement Tails (in Z events) well understood (SM backgrounds, mis-measured jets) QCD background not shown in the plots: ~ 1% in Z events, ~ 2-3% in W events

fmiss distribution Zee Wen ATLAS Preliminary ATLAS Preliminary V ATLAS ITALIA - Rosa Simoniello fmiss very sensitive to all problems/non-uniformities in calorimeters data-MC good agreement (improvements in rel16, data and MC have cell coordinates updated to reflect the measured position of FCal). All ETmiss distributions shown are calculated in |h|<4.5 due a still not perfect description of FCal in MC. Distributions in |h|<4.5 are still better then the ones in |h|<5 which, however, show a big improvement.

ETmiss distributions of RefFinal terms (Zee) 2 balanced jets Electrons term 0 jets unbalanced jets pt>20GeV ATLAS Preliminary ATLAS Preliminary Jets pT>20GeV term Jets 7GeV<pT<20GeV term Cells in topoclusters outside objects V ATLAS ITALIA - Rosa Simoniello ATLAS Preliminary ATLAS Preliminary Good agreement data-MC

ETmiss distributions of RefFinal terms (Zµµ) Calo muon term Muon term ATLAS Preliminary ATLAS Preliminary V ATLAS ITALIA - Rosa Simoniello Distribution of ETmiss computed with cells crossed by muons in calorimeter Distribution of ETmiss computed from reconstructed muons Good agreement data-MC

Diagnostic plot (Z events) pT(Z) Longitudinal axis Hadronic recoil Perpendicular axis ETmiss ATLAS Preliminary Zµµ ETmiss should be balanced along the longitudinal axis ETmiss along longitudinal axis has a negative bias for low values of pTZ, probably due to underestimation of hadronic recoil imperfections in CellOut and SoftJets terms calibration CellOut improved with tracks (black dots) reduces the bias in events where there are no jets with pT>7GeV V ATLAS ITALIA - Rosa Simoniello ATLAS Preliminary

Resolution curves Data MC V ATLAS ITALIA - Rosa Simoniello On x-axis there’s the ∑ET of the whole event (calo+muon). For W events the resolution is calculated only for MC because it is necessary the ETmiss,truth value. Leptons are better measured: Z events (two leptons) has a better resolution then W events (one lepton) which have a slightly better resolution then MinBias and QCD events.

Linearity Wen Wµn Linearity from MC W events ATLAS Preliminary ATLAS Preliminary V ATLAS ITALIA - Rosa Simoniello Linearity from MC W events ETmiss,reco is positive by definition, so the linearity is negative for ETmiss values near 0GeV (<40GeV) Due to the finite detector resolution linearity distributions show a displacement from 0: Wen  at most 1% Wµn at most 4% (tune better the contribution of muons in calo?)

∑ET distribution Not yet published by ATLAS Pythia MC10 (now) Pythia MC09 (last year) Pythia8 (CMS tune) V ATLAS ITALIA - Rosa Simoniello Not yet published by ATLAS Pythia MC09  mismodelling in the soft physics Pythia MC10  new tune to increase the underline event activity  improvements in data-MC agreements Pythia8 (used by CMS)  Lower statistics available => compared with data from only one run  good agreement data-MC but still not perfect

Etmiss Systematics Systematic uncertainty from MC V ATLAS ITALIA - Rosa Simoniello Systematic uncertainty from MC Systematic uncertainty from topoclusters energy scale uncertainty Etmiss Systematics

ETmiss Systematic Uncertainty The refined ETmiss makes use of reconstructed objects, so its systematic uncertainty can be calculated from the uncertainty on each high-pt reconstructed objects (provided by CP ATLAS groups) and from the uncertainty on SoftJets and CellOut terms. The contribution of each term varies for different channels in Z and W events the contribution of SoftJets and CellOut is important. What is done in the CONF note: Evaluation of systematic uncertainty on SoftJets and CellOut term: same approach as for evaluation of JES uncertainty: systematic uncertainties from various sources estimated with MC dedicated simulation same approach as for W/Z cross-section paper: systematic uncertainty on SoftJets and CellOut is evaluated from the topocluster energy scale uncertainty V ATLAS ITALIA - Rosa Simoniello 23

Systematic Uncertainty on CellOut and SoftJets terms Evaluation from MC Evaluation from topocluster energy scale uncertainty (very conservative estimation to be improved) Used MC with different dead material description, shower models, underlying event and FSR Shift topocluster energy scale with the formula: V ATLAS ITALIA - Rosa Simoniello CellOut Uncertainty ~ 13% combining with MC uncertainties: CellOut Uncertainty ~ 13.2% < 1 % on RefFinal It gives an uncertainty on CellOut term of 2.6%. In the same way, on SoftJets term we get SoftJets Uncertainty ~ 10.5%  < 0.5 % on RefFinal

Systematic Uncertainty on CellOut and on RefFinal Impact of CellOut on RefFinal ATLAS Preliminary ATLAS Preliminary V ATLAS ITALIA - Rosa Simoniello Despite the uncertainty on SoftJets and CellOut terms are quite large (due to a very conservative estimation) , their effect on the whole ETmiss RefFinal is small In Top and SUSY events (where SoftJets and CellOut terms have a smaller contribution than the ones in W events) the impact on the RefFinal systematics uncertainty is smaller Systematic uncertainty on LCW Jets given yesterday by jet group

V ATLAS ITALIA - Rosa Simoniello MT method Etmiss SCAlE

ETmiss Scale ETmiss scale results in agreement with Linearity results ETmiss scale determined from the study of the shape of the lepton-neutrino transverse mass distribution in W → lν events Method sensitive to both ETmiss scale (a) and resolution (s) ETmiss,true (pTn) scaled and smeared Estimate background by fit data using a linear combination of signal and background MT distributions obtained from the MC simulation (Ratio of Electroweak background fixed through ratio of cross sections) V ATLAS ITALIA - Rosa Simoniello ETmiss scale results in agreement with Linearity results Only statistical uncertainty Systematic uncertainty ~ 1% => Total uncertainty ~ 2%

Conclusions From validation plots in the last CONF note the RefFinal calibration is recommend for physical analysis in data 2010 The fmiss and ∑ET distributions show improvements The systematics uncertainties for CellOut and softjets terms are also provided. A first and preliminary evaluation of the ETmiss absolute scale is done in-situ using W events. Ongoing V ATLAS ITALIA - Rosa Simoniello Tool to provide MET_RefFinal systematic uncertainty Study of the pileup in data 2011 Move the Milano group in the A/Htt analysis where the ETmiss performance are crucial in invariant mass reconstruction (see Sofia’s talk) Frascati group: optimization of the eflow algorithm and determination of Etmiss scale with data 2011

Back up V ATLAS ITALIA - Rosa Simoniello

Topoclusters Topo-Clusters are groups of calorimeter cells topologically connected Noise suppression via noise-driven clustering thresholds: Seed, Neighbour, Perimeter cells (S,N,P) = (4,2,0) seed cells with |Ecell| > Sσnoise (S = 4) expand in 3D; add neighbours with |Ecell|>Nσnoise (N = 2) merge clusters with common neighbours add perimeter cells with |Ecell|>Pσnoise (P = 0) V ATLAS ITALIA - Rosa Simoniello

Local cluster weighting calibration scheme (Local hadronic calibration or LCW) Local Hadron Calibration classifies calorimeter clusters as hadronic and electromagnetic, according to cluster topology and weights each cell in clusters according to the cluster energy, the cell energy density, the pseudorapidity, the isolation and the depth in calorimeter. Additional corrections are applied for energy deposited in calorimeters outside of clusters and the energy deposited in dead material. Finally, for the proper jet calibration, a pT and h dependent correction is applied to reach the calibrated jet energy scale. V ATLAS ITALIA - Rosa Simoniello

RefFinal Calibrations Configuration eg RefMuon Jet (pt>20GeV) Softjets (7GeV<pt<20GeV) CellOut Tau RefFinal default STACO AntiKt6 LCW+JES AntiKt6 LCW LCW+eflow RefFinal_em Muid AntiKt4 EM+JES AntiKt4 EM RefFinal_GCW GCW+JES GCW RefFinal_LCW RefFinal_noTracks LCW+JES V ATLAS ITALIA - Rosa Simoniello

Data and Montecarlo samples used DATA 2010: periods F-I ~36pb-1 --7 TeV e/g and muon Streams - W/Z official skims - JetEtmiss D3PD GRL inclusive for both electron and muon analysis At least 1 good primary vertex, |vxp_z|<200mm, with Ntrack>=3 Jet-Cleaning : remove events with at least 1 jet with pT>20 GeV with Antikt6TopoEM_IsBadMedium=1 (do not use jets if DR<=0.4 with electrons) MONTE CARLO Pythia MC10 --Z/W events 100 + 100 Kevts/ 140+140 Kevts events with in-time pileup re-weight to match the number of vertex distribution in data --tt, WW, WZ, Wtn for background evaluation --Minimum Bias for resolution comparison 33

Zll selection “similar” to the ones adopted for Z analysis in rel16 Trigger Muon Data: Period F-G1 (runs 162347 to 165632) : EF_mu10_MG Period G2-I1 (up to run 16757) : EF_mu13_MG Period I1 (from run 167607) - I2 : EF_mu15 Muon MC: EF_mu10_MG Electron Data: EF_e15_medium Electron MC Z mm: exactly 2 good muons of opposite charge Combined muons, pT>20GeV and |h|<2.5 Cuts on number of hits used to reconstruct inner track z displament from vertex <10mm Isolation: ptcone20/pt<0.1. Zee: exactly 2 electrons of opposite charge ElectronMedium_WithTrackMatch electrons with pT>=20 GeV and |h|<=2.47 not in cracks Remove electron clusters if in OTX Z reconstructed mass in 66-116 GeV ~9000 Zee events and ~13000 Zmm events in data (~2% background expected) ~27000 Zee events and ~36000 Zmm events in MC 34

Wln selection “similar” to the ones adopted for Z analysis in rel16 Muons: use same criteria as Zmm Electrons: use ElectronTight_WithTrackMatch and Isolation: Etcone40/Et<0.5. Di-lepton veto applied - no other electrons medium pT>10 - no muon combined EtMiss>25GeV mT (lepton-EtMiss)>50 GeV ~85000 Wen events and ~105000 Wmn events selected in data (~5% background expected) ~40000 Wen events and ~51000 Wmn events selected in MC 35

Systematic uncertainty on RefJet Systematic uncertainty on RefJet ~ 3-4% => on RefFinal: ~ 1% slightly increasing with ∑ET in agreement with the ones obtained by jet group