JULIeT JULIeT ( ( J J ava-based ava-based U U HE HE L L epton epton I I nt nt e e gral gral T T ransporter) ransporter) Motivation Motivation Java class structure Java class structure What you can do What you can do The version 1.0 release The version 1.0 release Shigeru Yoshida Shigeru Yoshida Dept. of Physics Dept. of Physics CHIBA Univ. CHIBA Univ. Bartol 2004
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JULIeT (Java-based UHE Lepton Integral Transporter) Motivation Motivation Java class structure Java class structure What you can do What you can do The.
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Published in Phys. Rev. DPublished in Phys. Rev. D S.Yoshida, R.Ishibashi, H,Miyamoto, PRD 69 (2004)S.Yoshida, R.Ishibashi, H,Miyamoto, PRD 69 (2004)
90% C.L. for 10 year observation
Bartol 2004
Monte Carlo modeMonte Carlo mode
Energy deposit profile in kmEnergy deposit profile in km33
By the JULIeT Monte Carlo functionBy the JULIeT Monte Carlo function
Bartol 2004
Version 1.0 releasedVersion 1.0 released
http://www.ppl.phys.chiba-u.jp/JULIeT/http://www.ppl.phys.chiba-u.jp/JULIeT/ The detailed USERS MANUAL availableThe detailed USERS MANUAL available The API Documents The API Documents The Swing-based GUI availableThe Swing-based GUI available Open for EVRYBODY. Visit our web site!Open for EVRYBODY. Visit our web site! Next step: Hook this up to the IceTray/PhotNext step: Hook this up to the IceTray/Phot
onicsonics
Backup SilidesBackup Silides
Laguna Beach 2003
The Whole Structure
Java_lib
sources
classes
icecube UHE
particles
points
interactions decay
propagation
numRecipes
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particles/
Defines particles with mass, lifetime, and energy
flavor
doublet
0
0
1
1 2 3
e
e 0
+
10 GeV < E < 10 GeV6 11(Initial. Changeable)
Particle.java ParticleArray.java
Laguna Beach 2003
points/ParticlePoint.java
•Define/calculate the point vector to trace particles•Define/calculate the medium(Rock/Ice) in which particles travel
density, mass number, charge, . . .
In Future. . .
Xxxx.javaTake the configuration of the Antarctica Ice
Laguna Beach 2003
interactions/
Interactions.java (abstract)•Total/differential cross sections•Integral differential cross sections•Integral inelasticity term