Detecting Cosmic Rays with LOFAR - LOFAR Community Science Workshop 2019
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Detecting Cosmic Rays with LOFAR LOFAR Community Science Workshop 2019 Katie Mulrey for the CR KSP A. Bonardi, S. Buitink, A. Corstanje, H. Falcke, B. M. Hare, J. R. Hörandel, T. Huege, G. Krampah, P. Mitra, K. Mulrey*, A. Nelles, H. Pandya, J. P. Rachen, L. Rossetto, P. Schellart, O. Scholten, S. ter Veen S. Thoudam, T. N. G. Trinh, T. Winchen 1 *kmulrey@vub.be
Cosmic Rays and Multi-Messenger Astronomy ν p γ Gamma rays: point to sources, can be absorbed, multiple emission mechanisms Neutrinos: point to sources, not absorbed, weak interaction Cosmic rays: charged and deflected, info in composition, easy to detect
Cosmic ray all-particle spectrum Galactic transition? extra galactic G. Matthiae et al. New J. Phys 12 (2010) 2
Cosmic ray energy & composition Galactic: SNR Extragalactic: AGN Hillas criterion: Emax ∝ Z e B r Max Energy EFe, max= 26 x Ep,max • Below 1019 eV, can’t point IceCube Masterclass 2019 directly to sources • Use composition to understand origin • Transition to heavier composition indicates the maximum source energy is reached 3
Composition: Measuring Xmax Xmax is an observable that gives radio detection information about composition nearly 100% duty cycle LOFAR, AERA, Tunka T. Huege. Physics Reports, 620:1-52,2016 fluorescence light dark nights (
Cosmic ray radio emission Geomagnetic Charge Excess Radiation Pattern: • Direction • Magnetic Field • Energy • Xmax • Atmosphere 5
Cosmic Ray Detection at LOFAR • LOFAR Radboud Array • scintillator detectors • Provides trigger for antenna readout 300 m offline analysis trigger buffer 2 ms read-out • RFI cleaning • direction reconstruction • antenna pattern unfolding • calibration P. Schellart et al., A&A 560, 98 (2013) 6 LBA stations (6 x 48 antennas) + stations outside Superterp 7
Stokes Parameters Geomagnetic Charge Excess vxvxB vxvxB vxB + vxB Pim Schellart et al., JCAP 10 14 (2014) I Q U V O. Scholten et al., PRD 94 1030101 (2016) 8
ucted from the arrival times of the nnas), and for each antenna polar- Stokes Parameters he form of the Stokes parameters: V. The orientation of the polar- tructed from Stokes Q and U. tween June 2011 and September corded a total of 762 air show- intensity pattern on the Charge Excess complexGeomagnetic G. Trinh et al PRD 95 083004 (2017) measured showers can be well re- vxvxB vxvxB ricate details by state of the art codes [22, 23]. These codes aug- nte Carlo air shower simulations alculated from first principles vxB +at vxB 11, 24]. In this analysis we use CORSIKA [25] with QGSJETII m ! or s the hadronic interaction models. y that the exact shape of the pat- r s t d e istance to the shower maximum, u n Pim Schellart et al., Th JCAP 10 14 (2014) bsolute field strength scales with y of the primary particle. owers cannot be correctly repro- Of these, 27 air showers have a se ratio below ten in amplitude et a reliable reconstruction. For wers three additional I observations Q U V he showers occur within two hours orded by the Royal Dutch Meteo- MI). Moreover, their polarization antly from that of a ‘normal’ fair- his can be seen in Fig. 1. For air- O. Scholten et al., PRD 94 1030101 (2016) 8 g thunderstorm conditions the po-
Event Analysis Radiation from track endpoints CoREAS simulation • no assumptions about emission SB et al. PRD 90 082003 (2014). • independent of LOFAR data hadronic models • 200-450 antennas / T. Huege et al. AIP Conf.Proc. 1535 (2013) no.1, 128 event • Total power within 55ns of peak emission 9
Event Analysis • Simulate proton and iron showers Preliminary Proton • Power scales with energy2 See talk by • Calculate reduced X2 for each A. Corstanje simulation • Parabola fit determines event Xmax • Resolution < 20 g/cm2 • Best fit (2016): 80% light particles Iron (p+He) at 1017 -1017.5 eV 10
GDAS Atmospheric Corrections • GDAS provides atmosphere measurements (temp, humidity, pressure) • Any location (1˚x1˚), time (3-hourly) • Integrated into simulations • For extreme conditions, can shift Xmax up to 15 g/cm2 A. Corstanje Astropart.Phys. 89 (2017) P. Mitra et al. PoS ICRC2017 (2018) 325 12
Calibration 13
Calibration 14
Calibration Buffer boards! LFmap 5
Calibration sky model K. Mulrey et al. Astropart.Phys 111 (2019) 1-11. 16
LORA expansion • Current cosmic-ray trigger is based on 20 Current LORA scintillators on the superterp • Expand by adding 20 scintillators at neighboring • Expected 45% increase in events Installation began spring 2018 17
Low Energy Extension: Hybrid Trigger Buitink et al., 2016 Proton Iron All CR primaries must have same probability of triggering to remove bias Current trigger 18
Hybrid Trigger Particle trigger - High rate with low trigger threshold Cosmic ray - Composition bias at low energies + + Guaranteed cosmic ray good radio signal + Radio trigger RFI rejection - Flooded with RFI + + Ensures a usable CR signal Reduced trigger threshold 19
Hybrid Trigger CR detectable with radio Trigger rate (Hz) Event with high RFI Min # detectors triggered Bias-free detection down to 1016.2 eV Current detection criteria Need access to existing radio trigger info in real time to form trigger 20
G. Matthiae et al. New J. Phys 12 (2010) Can we access the highest energy particles? !22 21
Goldstone VLA Westerbork Lovell ATCA Kalyazin LOFAR Parkes !23 22
T. Winchen !24 23
T. Winchen 24
25
Summary • LOFAR measures air showers with highest precision in radio • Xmax reconstruction resolution competitive with fluorescence • New atmospheric modelling & calibration • Multiple Extensions (hybrid trigger + LORA) • Lunar detection very promising (overlap with ground experiments!) 27
Backup
Calorimetric Energy Estimate Radio emission from cosmic rays provides a calorimetric energy measurement without uncertainties from hadronic models Glaser et al. JCAP 1609 (2016) Integrate fluence of radio footprint RD 11
T. Winchen
nalysis a number of physical param- and stored. These include the esti- Thunderstorm events e air shower (as reconstructed from r data), the arrival direction of the structed from the arrival times of the LOPES: ntennas), Amplification and for in thunderstorms each antenna polar- S.B. et al. A&A 467, 385 (2007) in the form of the Stokes parameters: and V. The orientation of the polar- onstructed LOFAR:from Stokes Q and U. measure atmospheric E-field between June 2011Schellart and September et al. PRL 114, 165001 (2015) recorded a total of 762 air show- Trinh et ted complex intensity pattern onal. thePRD 93, 023003 (2016) ll measured showers can be well re- intricate details by state of the art on codes [22, 23]. These codes aug- Monte Carlo air shower simulations n calculated from first principles at el [11, 24]. In this analysis we use n of CORSIKA [25] with QGSJETII 7] as the hadronic interaction models. usly that the exact shape of the pat- e distance to the shower maximum, e absolute field strength scales with ergy of the primary particle. showers cannot be correctly repro-
Hillas Plot J. Aguilar, ULB
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