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IceCube simulation with PPC Dmitry Chirkin, UW Madison, 2010 effective scattering coefficient (from Ryan Bay)

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Presentation on theme: "IceCube simulation with PPC Dmitry Chirkin, UW Madison, 2010 effective scattering coefficient (from Ryan Bay)"— Presentation transcript:

1 IceCube simulation with PPC Dmitry Chirkin, UW Madison, 2010 effective scattering coefficient (from Ryan Bay)

2 Direct photon tracking with PPC simulating flasher/standard candle photons same code for muon/cascade simulation using Henyey-Greenstein scattering function with =0.8 using tabulated (in 10 m depth slices) layered ice structure employing 6-parameter ice model to extrapolate in wavelength transparent folding of acceptance and efficiencies precise tracking through layers of ice, no interpolation needed much faster than photonics for E -2 nugen and unweighted CORSIKA:  1000 corsika files (4 sec each) in 24.5 hours  2500 E -2 nugen files in 24.5 hours IC-40 i.e., 10000 E -2 nugen files in ~3-4 days on 6-GPU cudatest

3 Photon Propagation Code: PPC There are 5 versions of the ppc: original c++ "fast" c++ in Assembly for CUDA GPU icetray module All versions verified to produce identical results Also compares well with Tareq’s i3mcml (Mary Murphy’s results) http://icecube.wisc.edu/~dima/work/WISC/ppc/

4 Ice Fitting with PPC It became obvious that the AHA ice parameterization is inaccurate in explaining the IceCube data (flasher, standard candles, muon background, atmospheric neutrino, more?) and a new direct fitting procedure was implemented:  For each set of ice parameters (scattering and absorption at ~100 depths (10- meter slices in depth) the detector response was simulated to 60 different flasher events (on string 63). This response was compared to the data with a likelihood function, which took into account both statistical and 10% belt of systematic errors.  The minimum found with AHA as the initial approximation resulted in SPICE (South Pole Ice) model  The minimum found with bulk ice as the initial approximation but combined with the dust logger data to extrapolate in x and y for positions other than that of string 63, and in depth above and below the detector, resulted in SPICE 2 (South Pole Ice, second iteration) model  More iterations may be possible to take into account other sources of data

5 SPICE verification with CORSIKA by Anne Schukraft

6 Already much better agreement than with AHA! Some disagreement remains, more work is needed

7 SPICE simulation of  by Sean Grullon

8 At the horizon: no need for exotic neutrino interaction ideas

9 Summary 1.PPC is a direct photon propagation tool.  extensively verified  uncompromising precision of ice description  no interpolation  uses full xy map of ice properties  reached the production level of performance 2.SPICE 2 (South Pole ICE) model has been  fitted to IceCube flasher data collected on string 63 in 2008  demonstrated remarkable correlation with the dust logger data  therefore was extended to incorporate these data  use of flasher timing information is possible (under investigation) 3.Very good agreement is demonstrated with  background muon simulation  OM occupancies, COGz, Nch.  time residual slope vs. depth  neutrino simulation  Better agreement than AHA in COGz, Nch, energy estimators  Good agreement in COGz at the horizon


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