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1\section{Atmospheric Neutrinos}
2\label{sec:Phys-Atm-neut}
3%
4%\REDBLA{Creation by JEC 27/4/06 waiting for M. Maltoni Draft $\sim$22May}
5%\REDBLA{Update by JEC 22/6/06}
6%\REDBLA{Update by JEC 16/10/06: this is a section now}
7%\REDBLA{Update by AB + JEC 3/11/06 : subsectioning + tau-neutrinos}
8\subsection{Introduction}
9%%
10%use \refTab{} and \refFig{} commands to reference Tables and Figures.
11%JEC 22/6/06 START: contribution from Michele Maltoni
12Atmospheric neutrinos originates from the decay chain initiated by the
13collision of cosmic rays with the upper layers of the Earth's
14atmosphere.
15%
16\begin{figure}
17    \includegraphics[width=\columnwidth]{./figures/fig.octant.eps}
18    \caption{ \label{fig:octant} %
19      Discrimination of the wrong octant solution as a function of
20      $\sin^2\theta_{23}^\mathrm{true}$, for
21      $\theta_{13}^\mathrm{true} = 0$. We have assumed 10 years of
22      data taking with a 440-kton detector.}
23\end{figure}
24The hadronic interaction between primary cosmic rays (mainly protons
25and helium nuclei) and the light atmosphere nuclei produces secondary
26$\pi$ and $K$ mesons, which then decay giving electron and muon
27neutrinos and antineutrinos.
28%
29At lower energies the main contribution comes from $\pi$ mesons, and
30the decay chain $\pi \to \mu + \nu_\mu$ followed by $\mu \to e + \nu_e
31+ \nu_\mu$ produces essentially two $\nu_\mu$ for each $\nu_e$.  As
32the energy increases, more and more muons reach the ground before
33decays, and therefore the $\nu_\mu / \nu_e$ ratio increases.
34%
35For $E_\nu \gtrsim 1$~GeV the dependence of the total neutrino flux on
36the neutrino energy is well described by a power law, $d\Phi / d_E
37\propto E^{-\gamma}$ with $\gamma = 3$ for $\nu_\mu$ and $\gamma=3.5$
38for $\nu_e$, whereas at sub-GeV energies the dependence becomes more
39complicated because of the effects of the solar wind and of the
40Earth's magnetic field~\cite{Gonzalez-Garcia:2002dz}. As for the
41zenith dependence, for energies larger than a few GeV the neutrino
42flux is enhanced in the horizontal direction since pions and muons can
43travel a longer distance before reaching the ground, and therefore
44have more chances to decay producing neutrinos.
45
46Historically, the atmospheric neutrino problem originated in the
471980's as a discrepancy between the atmospheric neutrino flux measured
48with different experimental techniques. In the previous years, a
49number of detectors had been built, which could detect neutrinos
50through the observation of the charged lepton produced in
51charged-current neutrino-nucleon interactions inside the detector
52itself.
53%
54These detectors could be divided into two classes: \emph{iron
55calorimeters}, which reconstructed the track or electromagnetic shower
56produced by the lepton, and \emph{water \v{C}erenkov}, which measured
57instead the Cerenkov light emitted by the lepton as it moved faster
58than light in water.
59%
60The oldest iron calorimeters, Frejus \cite{Daum:1994bf} and
61NUSEX \cite{Aglietta:1988be}, found no discrepancy between the
62observed flux and the theoretical predictions, whereas the two \WC\ detectors, IMB \cite{Becker-Szendy:1992hq} and
63Kamiokande \cite{Hirata:1992ku}, observed a clear deficit in the
64predicted $\nu_\mu / \nu_e$ ratio.
65%
66The problem was finally solved in 1998, when the water Cerenkov
67detector SuperKamiokande \cite{Fukuda:1998mi} established with high
68statistical accuracy that there was indeed a zenith- and
69energy-dependent deficit in the muon neutrino flux with respect to the
70theoretical predictions, and that this deficit was compatible with the
71hypothesis of mass-induced $\nu_\mu \to \nu_\tau$ oscillations. Also,
72the independent confirmation of this effect from the iron calorimeter
73experiments Soudan-II \cite{Allison:1999ms} and
74MACRO \cite{Ambrosio:2001je} eliminated the discrepancy between the
75two experimental techniques.
76
77Despite providing the first solid evidence for neutrino oscillations,
78atmospheric neutrino experiments have received only minor
79consideration during the last years. This is mainly due to two
80important limitations:
81%
82\begin{itemize}
83  \item the sensitivity of an atmospheric neutrino experiments is
84    strongly limited by the large uncertainties in the knowledge of
85    neutrino fluxes and neutrino-nucleon cross-section. Such
86    uncertainties can be as large as 20\%.
87   
88  \item in general, water Cerenkov detectors do not allow an accurate
89    reconstruction of the neutrino energy and direction if none of the
90    two is known ``a priori''. This strongly limits the sensitivity to
91    $\Delta m^2$, which is very sensitive to the resolution on $L/E$.
92\end{itemize}
93%
94During its phase-I, Super-Kamiokande has collected 4099 electron-like
95and 5436 muon-like contained neutrino events \cite{Ashie:2005ik}. With
96only about a hundred events each, K2K \cite{Ahn:2006zz} and
97MINOS \cite{Tagg:2006sx} already provide a stronger bound on the
98atmospheric mass-squared difference $\Delta m_{31}^2$. The present
99value of the mixing angle $\theta_{23}$ is still dominated by
100Super-Kamiokande data, being statistics the most important factor for
101such a measurement, but strong improvements are expected from the next
102generation of long-baseline experiments T2K \cite{Itow:2001ee} and
103NO$\nu$A \cite{Ayres:2004js}.
104
105
106\begin{figure}
107    \includegraphics[width=\columnwidth]{./figures/SPLBBMEMPHYS-fig16.eps}
108    \caption{ \label{fig:hierarchy} %
109      Sensitivity to the mass hierarchy at $2\sigma$ ($\Delta\chi^2 =
110      4$) as a function of $\sin^22\theta_{13}^\mathrm{true}$ and
111      $\delta_\mathrm{CP}^\mathrm{true}$ (left), and the fraction of
112      true values of $\delta_\mathrm{CP}^\mathrm{true}$ (right). The
113      solid curves are the sensitivities from the combination of
114      long-baseline and atmospheric neutrino data, the dashed curves
115      correspond to long-baseline data only. We have assumed 10 years
116      of data taking with a 440-kton detector.}
117\end{figure}
118%
119\subsection{Oscillation physics}
120%
121Despite these drawbacks, atmospheric detectors can still play a
122leading role in the future of neutrino physics due to the huge range
123in energy (from 100~MeV to 10~TeV and above) and distance (from 20~km
124\begin{figure}
125    \includegraphics[width=\columnwidth]{./figures/fig.theta13.eps}
126    \caption{ \label{fig:theta13} %
127      Sensitivity to $\sin^22\theta_{13}$ as a function of
128      $\sin^2\theta_{23}^\mathrm{true}$ for LBL data only (dashed),
129      and the combination LBL+ATM (solid). In the left and central
130      panels we restrict the fit of $\theta_{23}$ to the octant
131      corresponding to $\theta_{23}^\mathrm{true}$ and $\pi/2 -
132      \theta_{23}^\mathrm{true}$, respectively, whereas the right
133      panel shows the overall sensitivity taking into account both
134      octants. We have assumed 8 years of LBL and 9 years of ATM data
135      taking with the T2HK beam and a 1~Mton detector.}
136\end{figure}
137to more than 12000~Km) covered by the data. This unique feature, as
138well as the very large statistics expected for a detector such as
139MEMPHYS ($20\div 30$ times the present SK event rate), will allow a
140very accurate study of \emph{subdominant modifications} to the leading
141oscillation pattern, thus providing complementary information to
142accelerator-based experiments. More concretely, atmospheric neutrino
143data will be extremely valuable for:
144%
145\begin{itemize}
146  \item resolving the octant ambiguity: although future LBL
147    experiments are expected to considerably improve the measurement
148    of the absolute value of the small quantity $D_{23} \equiv
149    \sin^2\theta_{23} - 1/2$, they will have practically no
150    sensitivity on its sign.  On the other hands, it has been pointed
151    out \cite{Kim:1998bv,Peres:1999yi} that the $\nu_\mu \to \nu_e$ conversion
152    signal induced by the small but finite value of $\Delta m_{21}^2$
153    can resolve this degeneracy. However, observing such a conversion
154    requires a very long baseline and low energy neutrinos, and
155    atmospheric sub-GeV electron-like events are particularly suitable
156    for this purpose. In \refFig{fig:octant} we show the potential
157    of different ATM+LBL experiments to exclude the octant degenerate
158    solution.
159
160  \item resolving the hierarchy degeneracy: if $\theta_{13}$ is not
161    too small, matter effect will produce resonant conversion in the
162    $\nu_\mu \leftrightarrow \nu_e$ channel for neutrinos
163    (antineutrinos) if the mass hierarchy is normal (inverted). The
164    observation of this enhanced conversion would allow the
165    determination of the mass hierarchy. Although a magnetized
166    detector would be the best solution for this task, it is possible
167    to extract useful information also with a conventional detector
168    since the event rates expected for atmospheric neutrinos and
169    antineutrinos are quite different. This is clearly visible from
170    \refFig{fig:hierarchy}, where we show how the sensitivity to the
171    mass hierarchy of different LBL experiments is drastically
172    increased when the ATM data collected by the same detector are
173    also included in the fit.
174
175  \item measuring or improving the bound on $\theta_{13}$: although
176    atmospheric data alone are not expected to be competitive with the
177    next generation of long-baseline experiments in the sensitivity to
178    $\theta_{13}$, they will contribute indirectly by eliminating the
179    octant degeneracy, which is an important source of uncertainty for
180    LBL. In particular, if $\theta_{23}^\mathrm{true}$ is larger than
181    $45^\circ$ then the inclusion of atmospheric data will
182    considerably improve the LBL sensitivity to $\theta_{13}$, as can
183    be seen from the right panel of \refFig{fig:theta13} \cite{huber-2005-71}.
184
185%JEC 3/11/06 START place it at the end of the section
186%  \item searching for physics beyond the Standard Model: the appearance
187%    of subleading features in the main oscillation pattern can also be
188%    a hint for New Physics. The huge range of energies probed by
189%    atmospheric data will allow to put very strong bounds on
190%    mechanisms which predict deviation from the $1/E$ behavior. For
191%    example, the bound on non-standard neutrino-matter interactions
192%    and on other types of New Physics (such as violation of the
193%    equivalence principle, or violation of the Lorentz invariance)
194%    which can be derived from \emph{present} data is already the
195%    strongest which can be put on these
196%    mechanisms \cite{Gonzalez-Garcia:2004wg}. The increased statistics
197%    expected for MEMPHYS will further improve these constraints.
198%JEC 3/11/06 END
199\end{itemize}
200%
201%A Bueno 3/11/06 START new subsection
202\subsection{Direct detection of $\nu_\tau$ in the atmospheric neutrino flux}
203%
204At energies above a GeV,
205we expect unoscillated events to be upward-downward going symmetric.
206In contrast, we know that $\nu_\tau, \ \bar{\nu}_\tau$ induced events come from
207below the horizon (upward going events). Therefore
208the presence of $\nu_\tau$, $\bar{\nu}_\tau$ events can be revealed by a
209measured excess of upward going events.
210Hereafter we assume that the {$\nu_\mu$} and
211the {$\mathbf \nu_\tau$} are maximally mixed and their mass
212squared difference
213is {$ \Delta m^2 = 3. \times 10^{-3}$} eV{$^2$}.
214We use the Fluka 3D atmospheric neutrino fluxes.
215
216In GLACIER, the search for $\nu_\tau$ appearance is based on the
217information provided by the event kinematics and takes advantage
218of the special characteristics of $\nu_\tau$ CC and the subsequent
219decay of the produced $\tau$ lepton when compared to CC and NC interactions
220of $\nu_\mu$ and $\nu_e$, i.e. by making use of $\vec{P}_{candidate}$ 
221and $\vec{P}_{hadron}$. Due to the large background induced by the natural
222abundance of the atmospheric neutrino flux in $\nu_e$ and
223$\bar{\nu}_e$, we note that the measurement of a statistically
224significant excess of
225$\nu_\tau$ events is very unlikely for the $\tau \to e$ decay mode,
226therefore we conclude that a search
227based on this channel is hopeless. Same conclusions apply to
228the muonic decay channel.
229
230The situation is much more advantageous for the hadronic channels:
231we consider tau decays to one prong (single pion, rho) and to three
232prongs ($\pi^\pm \pi^0 \pi^0 $ and three charged pions).
233After a careful evaluation of the performance of different
234combinations of kinematic variables, we decided to use: $E_{visible}$,
235$y_{bj}$ (the ratio between the total hadronic energy and
236$E_{visible}$) and $Q_T$ (defined as the transverse momentum of the $\tau$
237candidate with respect to the total measured momentum). The chosen
238variables are not independent one from another but show
239correlations between them. These correlations can be exploited to reduce the
240background. In order to maximize the separation between signal
241and background, we use three dimensional likelihood functions
242${\cal L}(Q_T,E_{visible}, y_{bj})$ where
243correlations are taken into account. For every channel, we build three
244dimensional likelihood functions
245for both signal (${\cal L}^S_\pi, \ {\cal L}^S_\rho, \
246{\cal L}^S_{3\pi}$) and background (${\cal L}^B_\pi, \ {\cal L}^B_\rho, \
247{\cal L}^B_{3\pi}$). To enhance the separation of $\nu_\tau$ induced
248events from $\nu_\mu, \ \nu_e$ interactions, we take a ratio of
249likelihoods as the sole discriminant variable:
250\begin{equation}
251\ln \lambda_i \equiv \ln({\cal L}^S_i / {\cal L}^B_i)
252\end{equation}
253where $i=\pi,\ \rho, \ 3\pi$.
254
255To further improve the sensitivity of the $\nu_\tau$
256appearance search, we combine
257the three independent hadronic analyses into a single one.
258Events that are common to at least
259two analyses are counted only once and a survey of all possible
260combinations, for a restricted set of  values of the likelihood
261ratios, is performed. Table \ref{tab:combi} illustrates the
262statistical significance achieved by several selected combinations of the
263likelihood ratios for an exposure equivalent to 100 kton$\times$year.
264
265\begin{table}
266\caption{\label{tab:combi}Expected background and signal events for different
267combinations of the $\pi$, $\rho$ and $3\pi$ analyses. The considered
268statistical sample corresponds to an exposure of 100
269kton$\times$year. The best
270combination found is indicated in bold characters.}
271\begin{center}
272\begin{tabular}{cccclc}\hline\hline
273$\ln \lambda_\pi$ & $\ln \lambda_\rho$ & $\ln \lambda_{3\pi}$ & 
274Top & Bottom & $P_\beta$ ($\%$) \\
275Cut & Cut & Cut & Events & Events &  \\ \hline
2760. & 0.5 & 0. & 223 & $223 + 43 = 266$ & $2 \times 10^{-1}$ 
277($3.1\sigma$)\\
2781.5. & 1.5 & 0 & 92 & $92 + 35= 127$ & $2 \times 10^{-2}$ ($3.7\sigma$)\\
2793. & -1 & 0. & 87 & $87 + 33 = 120 $ & $3 \times 10^{-2}$ 
280($3.6\sigma$)\\
2813. & 0.5 & 0. & 25 & {$25 + 22= 47$}
282& {$2 \times 10^{-3}$ $(4.3\sigma)$} \\ 
2833. & 1.5 & 0 & 20 & $20 + 19 = 39$ & $4 \times 10^{-3}$ ($4.1\sigma$)\\
2843. & 0.5 & -1. & 59 & $59 + 30 = 89$ & $9 \times 10^{-3}$ ($3.9\sigma$)\\
2853. & 0.5 & 1. & 18 & $18 + 17 = 35$ & $1 \times 10^{-2}$ ($3.8\sigma$)\\ \hline\hline
286\end{tabular}
287\end{center}
288\end{table}
289The best combination, for a 100 kton$\times$year exposure,
290is achieved for the
291following set of cuts: {$\ln \lambda_\pi > 3$,
292$\ln \lambda_\rho > 0.5$} and {$\ln \lambda_{3\pi} > 0$}.
293The expected number of NC background events amounts to 25 (top)
294while 25+22 = 47 (bottom) are expected. $P_\beta$ is the Poisson probability
295for the measured excess of upward going events to be due to a
296statistical fluctuation as a function of the exposure. We have
297an effect larger than $4\sigma$ for an
298exposure of 100 kton$\times$year (one year of data taking with GLACIER).
299%A Bueno 3/11/06 START
300%
301% JEC 3/11/06 START new section
302\subsection{New phenomena beyond the "Standard Model"}
303%
304It is worth remembering that atmospheric neutrino fluxes are
305themselves an important subject of investigation, and at the light of
306the precise determination of the oscillation parameters provided by
307long-baseline experiments the atmospheric neutrino data accumulated by
308the proposed detectors can be used as a \emph{direct measurement} of the incoming
309neutrino flux, and therefore as an indirect measurement of the primary
310cosmic rays flux.
311
312The appearance
313    of subleading features in the main oscillation pattern can also be
314    a hint for New Physics. The huge range of energies probed by
315    atmospheric data will allow to put very strong bounds on
316    mechanisms which predict deviation from the $1/E$ behavior. For
317    example, the bound on non-standard neutrino-matter interactions
318    and on other types of New Physics (such as violation of the
319    equivalence principle, or violation of the Lorentz invariance)
320    which can be derived from \emph{present} data is already the
321    strongest which can be put on these
322    mechanisms \cite{Gonzalez-Garcia:2004wg}. So, the increased statistics
323    expected for the proposed detectors will further improve these constraints.
324% JEC 3/11/06 END
325%JEC 22/6/06 END
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