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Tau Neutrino Appearance via Neutrino Oscillations in Atmospheric ...

Tau Neutrino Appearance via Neutrino Oscillations in Atmospheric ...

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9Figure 1.3: A schematic view of the atmospheric neutr<strong>in</strong>o production. Cosmicrays hit the atmosphere of the Earth isotropically, and neutr<strong>in</strong>os are produced.<strong>Atmospheric</strong> neutr<strong>in</strong>os travel from 15 km to 13,000 km before reach<strong>in</strong>g thesurface of the earth.is def<strong>in</strong>ed to be the angle between the neutr<strong>in</strong>o direction and a l<strong>in</strong>e perpendicularto the ground. The cos<strong>in</strong>e of a zenith angle, cosθ = −1 corresponds tothe upward-go<strong>in</strong>g direction, cosθ = 0 to the horizontal direction, and cosθ =+1 to the downward-go<strong>in</strong>g direction. Further details of atmospheric neutr<strong>in</strong>osare described <strong>in</strong> Chapter 4.1.4.2 <strong>Neutr<strong>in</strong>o</strong> Oscillation ExperimentsThe first atmospheric neutr<strong>in</strong>o experiments were two water Cherenkov experiments,Irv<strong>in</strong>e-Michigan-Brookhaven (IMB) [22, 23] and Kamiokande [24,25]. Although their primary scientific goals were to search for proton decay

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