On the atmospheric neutrino oscillations, theta(13) and neutrino mass hierarchy

dc.contributor.areaPhysicsen_US
dc.contributor.authorPetcov, Serguey T.en_US
dc.contributor.authorPalomares-Ruiz, Sergioen_US
dc.contributor.departmentElementary Particle Theoryen_US
dc.date.accessioned2007-11-14T10:32:54Zen_US
dc.date.accessioned2011-09-07T20:26:39Z
dc.date.available2007-11-14T10:32:54Zen_US
dc.date.available2011-09-07T20:26:39Z
dc.date.issued2007-11-14T10:32:54Zen_US
dc.description.abstractWe give predictions for the up-down asymmetry in the Nadir angle dependence of the ratio Nmu/Ne of the rates of the mu-like and e-like multi-GeV events measured in water-Cerenkov detectors (Super-Kamiokande, etc.) in the case of 3-neutrino oscillations of the atmospheric nu_e (antinu_e) and nu_mu (antinu_mu), driven by one neutrino mass squared difference, |Delta m^2_{atm}| = |Delta m^2_{31}| ~ (2.0 - 3.0) 10^{-3} eV^2 >> Delta m^2_{21} = Delta m^2_{sol}. This ratio is particularly sensitive to the Earth matter effects in the atmospheric neutrino oscillations, and thus to the values of sin^2(theta13) and sin^2(theta23), theta13 and theta23 being the neutrino mixing angle limited by the CHOOZ and Palo Verde experiments and that responsible for the dominant atmospheric nu_mu -> nu_tau (antinu_mu -> antinu_tau) oscillations, respectively. It is also sensitive to the type of neutrino mass spectrum which can be with normal (Delta m^2_{atm} > 0) or with inverted (Delta m^2_{atm} < 0) hierarchy.en_US
dc.format.extent122809 bytesen_US
dc.format.mimetypeapplication/pdfen_US
dc.identifier.urihttps://openscience.sissa.it/handle/1963/2416en_US
dc.language.isoen_USen_US
dc.relation.ispartofseriesSISSA;38/2004/EPen_US
dc.relation.ispartofseriesarXiv.org;hep-ph/0406106v1en_US
dc.titleOn the atmospheric neutrino oscillations, theta(13) and neutrino mass hierarchyen_US
dc.typePreprinten_US
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