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\lecture { 9} { } { Percolation, Introduction to characteristic functions}
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\subsubsection { Application: Percolation}
We will now discuss another application of Kolmogorov's $ 0 - 1 $ -law, percolation.
\begin { definition} [\vocab { Percolation} ]
Consider the graph with nodes $ \Z ^ d $ , $ d \ge 2 $ , where edges from the lattice are added with probability $ p $ . The added edges are called \vocab [Percolation!Edge!open] { open} ;
all other edges are called
\vocab [Percolation!Edge!closed] { closed} .
More formally, we consider
\begin { itemize}
\item $ \Omega = \{ 0 , 1 \} ^ { \bE _ d } $ , where $ \bE _ d $ are all edges in $ \Z ^ d $ ,
\item $ \cF \coloneqq \text { product $ \sigma $ - algebra } $ ,
\item $ \bP \coloneqq \left ( p \underbrace { \delta _ { \{ 1 \} } } _ { \text { edge is open } } + ( 1 - p ) \underbrace { \delta _ { \{ 0 \} } } _ { \text { edge is absent closed } } \right ) ^ { \otimes \bE _ d } $ .
\end { itemize}
\end { definition}
\begin { question}
Starting at the origin, what is the probability, that there exists
an infinite path (without moving backwards)?
\end { question}
\begin { definition}
An \vocab { infinite path} consists of an infinite sequence of distinct points
$ x _ 0 , x _ 1 , \ldots $
such that $ x _ n $ is connected to $ x _ { n + 1 } $ , i.e.~the edge $ \{ x _ n, x _ { n + 1 } \} $ is open.
\end { definition}
Let $ C _ \infty \coloneqq \{ \omega | \text { an infinite path exists } \} $ .
\begin { exercise}
Show that changing the presence / absence of finitely many edges
does not change the existence of an infinite path.
Therefore $ C _ \infty $ is an element of the tail $ \sigma $ -algebra.
Hence $ \bP ( C _ \infty ) \in \{ 0 , 1 \} $ .
\end { exercise}
Obviously, $ \bP ( C _ \infty ) $ is monotonic with respect to $ p $ .
For $ d = 2 $ it is known that $ p = \frac { 1 } { 2 } $ is the critical value.
For $ d > 2 $ this is unknown.
% TODO: more in the notes
We'll get back to percolation later.
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\section { Characteristic Functions, Weak Convergence and the Central Limit Theorem}
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% Characteristic functions are also known as the \vocab{Fourier transform}.
%Weak convergence is also known as \vocab{convergence in distribution} / \vocab{convergence in law}.
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So far we have dealt with the average behaviour,
\[
\frac { \overbrace { X_ 1 + \ldots + X_ n} ^ { \text { i.i.d.} } } { n} \to \bE (X_ 1).
\]
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We now want to understand fluctuations from the average behaviour,
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i.e.\[
X_ 1 + \ldots + X_ n - n \cdot \bE (X_ 1).
\]
% TODO improve
The question is, what happens on other timescales than $ n $ ?
An example is
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\begin { equation}
\frac { X_ 1 + \ldots + X_ n - n \bE (X_ 1)} { \sqrt { n} }
\xrightarrow { n \to \infty } \cN (0, \Var (X_ i))
\label { eqn:lec09ast}
\end { equation}
Why is $ \sqrt { n } $ the right order?
Handwavey argument:
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Suppose $ X _ 1 , X _ 2 , \ldots $ are i.i.d.~with $ X _ 1 \sim \cN ( 0 , 1 ) $ .
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The mean of the l.h.s.~is $ 0 $ and for the variance we get
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\begin { IEEEeqnarray*} { rCl}
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\Var (\frac { X_ 1 + \ldots + X_ n - n \bE (X_ 1)} { \sqrt { n} } )
& =& \Var \left ( \frac { X_ 1+ \ldots + X_ n} { \sqrt { n} } \right )\\
& =& \frac { 1} { n} \left ( \Var (X_ 1) + \ldots + \Var (X_ n) \right ) = 1
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\end { IEEEeqnarray*}
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For the r.h.s.~we get a mean of $ 0 $ and a variance of $ 1 $ .
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So, to determine what \eqref { eqn:lec09ast} could mean, it is necessary that $ \sqrt { n } $
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is the right scaling.
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To make \eqref { eqn:lec09ast} precise,
we need another notion of convergence.
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This will be the weakest notion of convergence, hence it is called
\vocab { weak convergence} .
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This notion of convergence will be defined in terms of
characteristic functions of Fourier transforms.
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\subsection { Characteristic Functions and Fourier Transform}
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\begin { definition}
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\label { def:characteristicfunction}
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Consider $ ( \R , \cB ( \R ) , \bP ) $ .
The \vocab { characteristic function} of $ \bP $ is defined as
\begin { IEEEeqnarray*} { rCl}
\phi _ { \bP } : \R & \longrightarrow & \C \\
t & \longmapsto & \int _ { \R } e^ { \i t x} \bP (\dif x).
\end { IEEEeqnarray*}
\end { definition}
\begin { abuse}
$ \phi _ \bP ( t ) $ will often be abbreviated as $ \phi ( t ) $ .
\end { abuse}
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We have
\[
\phi (t) = \int _ { \R } \cos (tx) \bP (dx) + \i \int _ { \R } \sin (tx) \bP (dx).
\]
\begin { itemize}
\item Since $ |e ^ { \i t x } | \le 1 $ the function $ \phi ( \cdot ) $ is always defined.
\item We have $ \phi ( 0 ) = 1 $ .
\item $ | \phi ( t ) | \le \int _ { \R } |e ^ { \i t x } | \bP ( dx ) = 1 $ .
\end { itemize}
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\todo { Properties of characteristic functions}
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\begin { remark}
Suppose $ ( \Omega , \cF , \bP ) $ is an arbitrary probability space and
$ X: ( \Omega , \cF ) \to ( \R , \cB ( \R ) ) $ is a random variable.
Then we can define
\[
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\phi _ X(t) \coloneqq \bE [e^{\i t X}]
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= \int e^ { \i t X(\omega )} \bP (\dif \omega )
= \int _ { \R } e^ { \i t x} \mu (dx) = \phi _ \mu (t),
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\]
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where $ \mu = \bP \circ X ^ { - 1 } $ .
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\end { remark}
\begin { theorem} [Inversion formula] % thm1
\label { inversionformula}
Let $ ( \Omega , \cB ( \R ) , \bP ) $ be a probability space.
Let $ F $ be the distribution function of $ \bP $
(i.e.~$ F ( x ) = \bP ( ( - \infty , x ] ) $ for all $ x \in \R $ ).
Then for every $ a < b $ we have
\begin { eqnarray}
\frac { F(b) + F(b-)} { 2} - \frac { F(a) + F(a-)} { 2} = \lim _ { T \to \infty } \frac { 1} { 2 \pi } \int _ { -T} ^ T \frac { e^ { -\i t b} - e^ { - \i t a} } { - \i t} \phi (t) dt
\label { invf}
\end { eqnarray}
where $ F ( b - ) $ is the left limit.
\end { theorem}
% TODO!
We will prove this later.
\begin { theorem} [Uniqueness theorem] % thm2
\label { charfuncuniqueness}
Let $ \bP $ and $ \Q $ be two probability measures on $ ( \R , \cB ( \R ) ) $ .
Then $ \phi _ \bP = \phi _ \Q \implies \bP = \Q $ .
Therefore, probability measures are uniquely determined by their characteristic functions.
Moreover, \eqref { invf} gives a representation of $ \bP $ (via $ F $ )
from $ \phi $ .
\end { theorem}
\begin { refproof} { charfuncuniqueness}
Assume that we have already shown \autoref { inversionformula} .
Suppose that $ F $ and $ G $ are the distribution functions of $ \bP $ and $ \Q $ .
Let $ a,b \in \R $ with $ a < b $ .
Assume that $ a $ and $ b $ are continuity points of both $ F $ and $ G $ .
By \autoref { inversionformula} we have
\begin { IEEEeqnarray*} { rCl}
F(b) - F(a) = G(b) - G(a) \label { eq:charfuncuniquefg}
\end { IEEEeqnarray*}
Since $ F $ and $ G $ are monotonic, \autoref { eq:charfuncuniquefg}
holds for all $ a < b $ outside a countable set.
Take $ a _ n $ outside this countable set, such that $ a _ n \ssearrow - \infty $ .
Then, \autoref { eq:charfuncuniquefg} implies that
$ F ( b ) - F ( a _ n ) = G ( b ) - G ( a _ n ) $ hence $ F ( b ) = G ( b ) $ .
Since $ F $ and $ G $ are right-continuous, it follows that $ F = G $ .
\end { refproof}