\documentclass[reqno]{amsart}
\usepackage{hyperref}

\AtBeginDocument{{\noindent\small
\emph{Electronic Journal of Differential Equations},
Vol. 2015 (2015), No. 14, pp. 1--17.\newline
ISSN: 1072-6691. URL: http://ejde.math.txstate.edu or http://ejde.math.unt.edu
\newline ftp ejde.math.txstate.edu}
\thanks{\copyright 2015 Texas State University - San Marcos.}
\vspace{9mm}}

\begin{document}
\title[\hfilneg EJDE-2015/14\hfil Camassa-Holm shallow water systems]
{Global dissipative solutions for the two-component Camassa-Holm \\
shallow water system}

\author[Y. Wang, Y. Song \hfil EJDE-2015/14\hfilneg]
{Yujuan Wang, Yongduan Song}

\address{Yujuan Wang \newline
School of Automation, Institute of smart system and renewable energy,
Chongqing University, Chongqing 400044, China }
\email{iamwyj123456789@163.com}

\address{Yongduan Song \newline
School of Automation, Institute of smart system and renewable energy,
Chongqing University, Chongqing 400044, China}
\email{ydsong@cqu.edu.cn, Phone 0862365103001}

\thanks{Submitted September 3, 2013. Published January 19, 2015}
\subjclass[2000]{35L05, 35L65, 35L51}
\keywords{Two-component Camassa-Holm system; global solutions;
\hfill\break\indent  dissipative solutions}

\begin{abstract}
 This article presents a continuous semigroup of globally defined weak
 dissipative solutions for the two-component Camassa-Holm system.
 Such solutions are established by using a new approach based on
 characteristics a set of new variables overcoming the difficulties
 inherent in multi-component systems.
\end{abstract}

\maketitle
\numberwithin{equation}{section}
\newtheorem{theorem}{Theorem}[section]
\newtheorem{definition}[theorem]{Definition}
\allowdisplaybreaks

\section{Introduction}

We consider the two-component Camassa-Holm shallow water
system  (see \cite{c2,c7,f1})
\begin{equation}\label{eq1}
\begin{gathered}
 m_t +um_x +2u_x m-Au_x +\rho \rho _x =0,\quad t>0,\;x\in \mathbb{R}, \\
 m=u-u_{xx} ,\quad t>0,\;x\in \mathbb{R}, \\
 \rho _t +(u\rho )_x =0,\quad t>0,\;x\in \mathbb{R}.
 \end{gathered}
\end{equation}
Here  $A>0$ characterizes a linear underlying shear flow so that \eqref{eq1}
models wave-current interactions. The variable $u(x,t)$
represents the horizontal velocity of the fluid, and $\rho (x,t)$
is the  scalar density. This system appears in \cite{o1}; it was also derived
by Constantin and Ivanov in \cite{c7} in the context of shallow water theory. It is
an extension of the Camassa--Holm (CH), is  formally
integrable \cite{c2,c7,f1}, and also has a bi-Hamiltonian structure with  Hamiltonians
\[
H_1 =\frac{1}{2}\int \big({um+({\rho -1})^2}\big) dx
\]
and
\[
H_2 =\frac{1}{2}\int {\Big({u({\rho -1})^2+2u({\rho -1}
)+u^3+uu_x^2 -Au^2}\Big)} dx.
\]
For $\rho \equiv 0$, one obtains the classical CH equation, which models the
unidirectional propagation of shallow water waves over a flat bottom. It has
a bi-Hamiltonian structure \cite{c3} and is completely integrable \cite{c1,c4}.
The CH equation has attracted a lot of attention just because it has peaked
solitons \cite{c1,c8} and models wave breaking \cite{c1,c6}.
The presence of breaking
waves means the solution remains bounded while its slope becomes unbounded
in finite time \cite{c5,c6}. After wave breaking the solutions of the CH
equation can be continued uniquely as either globally conservative \cite{b1} or
globally dissipative solutions\cite{b2}.

System \eqref{eq1} is an integrable multi-component generalization
of the CH equation. System \eqref{eq1}
has a physical interpretation\cite{c7}, just like the CH equation,  has an
integrable structure \cite{f1}, and can be expressed as a flow \cite{h1}.
It has been shown that the two-component CH system is locally well-posed
with initial data $({u_0 ,\;\rho _0 })\in H^s\times
H^{s-1}$, $s>3/2$ \cite{g2}. The system also has global strong solutions
which blow up in finite time \cite{e1}. More interestingly, it possesses a global
continuous semigroup of weak conservative solutions \cite{w1,w2}. The goal of the
present paper is to construct a global continuous semigroup of weak
dissipative solutions for the two-component Camassa-Holm system \eqref{eq1}. It
should be stressed that system \eqref{eq1} is a multiple (rather than single)
component system in which the mutual effect between the components $u$ and
$\rho $ exits, making it quite challenging to address properties of the  solutions
 associated with the system.

To circumvent the difficulties coming from the two-component
coupling effect, we introduce a suitable characteristic and a new set of
independent and dependent variables to transfer the system \eqref{eq1} into a
semilinear hyperbolic system. By solving the corresponding semilinear system
which contains a discontinuous non-local source term but has bounded
directional variation, a global dissipative solution is derived. Then, by
mapping the solution of the semilinear system into the solution of original
system \eqref{eq1}, the problem is solved. Furthermore, it is proved
that the solutions actually construct a
semigroup.

The remainder of this article is organized as follows.
Section 2 is the introduction of the original system.
In Section 3, a transformation from the
original system to an equivalent semilinear system is conducted by applying
a new set of variables. The unique global solution of the equivalent
semilinear system is derived in Section 4 and then it is reversed to the weak
dissipative solution of the original system in Section 5, which constructs a
global continuous semigroup.

\section{The original system}

Let $G(x)=\frac{1}{2}e^{-| x |}$ and $\ast $ denotes
the spatial convolution such that  $G\ast f=({1-\partial ^2}
)^{-1}f$ for all $f\in L^2(\mathbb{R})$. System \eqref{eq1} can thus be
rewritten as a form of quasi-linear evolution equation
\begin{gather*}
 u_t +uu_x +\partial _x G\ast ({u^2+\frac{1}{2}u_x^2
-Au+\frac{1}{2}\eta ^2+\eta })=0,\quad t>0,\;x\in \mathbb{R}, \\
 \eta _t +u\eta _x +\eta u_x +u_x =0,\quad  t>0,\;x\in \mathbb{R},
 \end{gather*}
which can be further represented in the form
\begin{equation} \label{eq2}
\begin{gathered}
 u_t +uu_x +P_x =0,\quad  t>0,\;x\in \mathbb{R}, \\
 \eta _t +u\eta _x +\eta u_x +u_x =0,\quad  t>0,\;x\in \mathbb{R},
 \end{gathered}
\end{equation}
where $\eta =\rho -1$ and
$P=G\ast (u^2+u_x^2/2  -Au+\eta ^2 / 2  +\eta )$,
with the initial condition $({u_0 ,\eta _0 })\in H^1\times U$
with $U=L^2\cap L^\infty $. For smooth solutions, the total energy
\begin{equation} \label{eq3}
E(t)=\int_R {u^2} +u_x^2 +\eta ^2\,dx
\end{equation}
is constant in time. Indeed, by using the identity
$\partial _x^2 G\ast f=G\ast f-f$ and differentiating the two equations
 in \eqref{eq2} with respect to $x$ respectively, we have
\begin{equation}\label{eq4}
\begin{gathered}
 u_{xt} +uu_{xx} +u_x^2 -({u^2+\frac{1}{2}u_x^2 -Au+\frac{1}{2}\eta
^2+\eta })+P=0, \\
 \eta _{xt} +2u_x \eta _x +({u\eta _{xx} +\eta u_{xx} +u_{xx} })=0.
\end{gathered}
\end{equation}
Multiplying the first equation in \eqref{eq2} by $u$ and the second equation by
$\eta $, and multiplying the first one in \eqref{eq4} by $u_x $, we obtain the
following conservation laws
\begin{gather} \label{eq5}
\Big({\frac{u^2}{2}}\Big)_t +\Big({\frac{u^3}{3}}\Big)_x +uP_x =0, \\
\label{eq6}
\Big({\frac{u_x^2 }{2}}\Big)_t +({\frac{1}{2}uu_x^2
-\frac{1}{3}u^3+\frac{1}{2}Au^2})_x -\frac{1}{2}\eta ^2u_x -\eta u_x
+u_x P=0, \\
\label{eq7}
\Big({\frac{\eta ^2}{2}}\Big)_t +\eta ^2u_x +\eta u_x +u\eta \eta _x
=0.
\end{gather}
It then follows from \eqref{eq5}-\eqref{eq7} that
\[
\frac{d}{dt}E(t)=\frac{d}{dt}\int_S {({u^2+u_x^2 +v^2}
)} ({t,x})dx=0.
\]
Thus \eqref{eq2} possesses the $H^1$-norm conservation law given by
\[
\| z \|_{H^1} =\Big({\,\int_R {[ {u^2+u_x^2 +\eta ^2}
]dx} }\Big)^{1/2},
\]
where $z=({u,\eta })$. Since
$z=({u,\eta })\in H^1\times U$, Young's inequality ensures $P\in H^1$.

\begin{definition}\label{def1} \rm
By a solution of the Cauchy problem \eqref{eq2} we mean a
H\"{o}lder continuous function $z=z({t,x})$ defined on
$[{0,T} ]\times R$  with the following properties:
\begin{itemize}
\item[(i)] $z({t,\;\cdot })\in H^1\times [ {L^2\cap L^\infty }
]$ for each fixed $t$.

\item[(ii)] The map $t\to z({t,\cdot })$ is Lipschitz continuous
from $[0,T]$ to $L^2$, satisfying
\begin{equation}\label{eq8}
\begin{gathered}
 z_t =-uz_x -f(z), \\
 z({0,x})=\bar {z}(x),
 \end{gathered}
\end{equation}
where $z=({u,\eta })$, $z_x =({u_x ,\eta _x })$
and $f(z)=({P_x ,\;({\eta +1})u_x })$.
\end{itemize}
\end{definition}

\begin{definition} \label{def2}\rm
We call a solution of the Cauchy problem \eqref{eq2} a
dissipative solution if it satisfies the Oleinik type inequality
\[
u_x ({t,x}),\eta _x ({t,x})\le C({1+t^{-1}}), \quad t>0
\]
for some constant $C$ depending only on the norm of the initial data
$\| {\bar {z}} \|_{H^1} $ and its energy $E(t)$ in \eqref{eq3}
is a non-increasing function of time.
\end{definition}

\section{The equivalent semilinear system}

In this section, a transformation is conducted by introducing a
characteristic and a new set of Lagrangian variables, with which the
original system is transformed into an equivalent semilinear hyperbolic
system.

For given initial data $\bar {z}=({\bar {u},\bar {\eta }})\in
H^1\times U$, we consider the following initial problem,
\begin{equation}\label{eq9}
\begin{gathered}
 \frac{\partial }{\partial t}q({t,\xi })=u({t,q({t,\xi })}),\quad t\in [ 0,T ], \\
 q({0,\xi })=\bar {q}(\xi),\quad x\in \mathbb{R},
 \end{gathered}
\end{equation}
where the solution $z=({u,\eta })$ to  \eqref{eq2} remains
Lipschitz continuous for $t\in [0,T]$, and the non-decreasing
maps $\xi \mapsto \bar {q}(\xi)$ is defined as
\begin{equation} \label{eq10}
\int_0^{\bar {q}(\xi)} {\bar {u}_x^2 } dx=\xi .
\end{equation}
The following notation is used:
\begin{gather*}
u({t,\;\xi })=u({t,\;q({t,\xi })}), \quad
\eta ({t,\;\xi })=\eta ({t,\;q({t,\xi })}), \quad
P({t,\;\xi })=P({t,\;q({t,\xi })}), \\
u_x ({t,\;\xi })=u_x ({t,\;q({t,\xi })}),\quad
\eta _x ({t,\;\xi })=\eta _x ({t,\;q({t,\xi })}), \quad
P_x ({t,\;\xi })=P_x ({t,\;q({t,\xi })}).
\end{gather*}
Define the variables $\theta =\theta ({t,\xi })$ and $w=w({t,\xi })$ as
\begin{equation}
\label{eq11}
\theta =2\operatorname{arcsec} u_x ,
\quad
w=u_x^2 \cdot \frac{\partial q}{\partial \xi }.
\end{equation}
($\theta $ in  $[ {0,\pi })\cup ({\pi ,2\pi } ])$.

We remark that the transformed variable $\theta $ used in this
paper is of the form $\theta =2\operatorname{arcsec} u_x $, which makes the calculation
much simple and convenient to set up the dissipative solution in contrast to
the applied variable $v=2\arctan u_x $ in \cite{b1,b2}, which further overcomes
the difficulties existing in the multi-component system.

The following useful identities are prepared for later use from
\eqref{eq9}-\eqref{eq11},
\begin{gather} \label{eq12}
w({0,\xi })\equiv 1, \\
\label{eq13}
u_x =\sec \frac{\theta }{2}, \quad
\frac{1}{u_x^2 }=\cos ^2\frac{\theta }{2}, \\
\label{eq14}
\frac{\partial q}{\partial \xi }=\frac{w}{u_x^2 }
=\cos ^2\frac{\theta }{2}\cdot w.
\end{gather}
According to \eqref{eq14}, we obtain
\begin{equation} \label{eq15}
q({t,{\xi }'})-q({t,\xi })=\int_\xi ^{{\xi }'}
{\cos ^2\frac{\theta }{2}({t,s})\cdot w} ({t,s})ds.
\end{equation}
By using the new variable $\xi $, we represent $P$ and $P_x $ as follows,
\begin{align*}
P(\xi)&=\frac{1}{2}\int_{-\infty }^{+\infty } {\exp \Big\{
{-\big| {\int_\xi ^{{\xi }'} {\cos ^2} \frac{\theta (s
)}{2}\cdot w(s)ds} \big|} \Big\}} \\
&\times \big[ {\big({u^2-Au+\frac{1}{2}\eta ^2+\eta }\big)\cos
^2\frac{\theta }{2}+\frac{1}{2}} \big] w({{\xi }'})d{\xi}',
\end{align*}
\begin{equation} \label{eq16}
\begin{aligned}
P_x (\xi)
&=\frac{1}{2}\Big({\int_\xi ^{+\infty }
{-\int_{-\infty }^\xi } }\Big)\exp \Big\{ {-\big| {\int_\xi ^{{\xi }'}
{\cos ^2} \frac{\theta (s)}{2} w(s)ds}
\big|} \Big\}\\
&\quad\times \big[ {\big({u^2-Au+\frac{1}{2}\eta ^2+\eta }\big)\cos
^2\frac{\theta }{2}+\frac{1}{2}} \big] w({{\xi }'})d{\xi}',
\end{aligned}
\end{equation}
System \eqref{eq2} can be further rewritten with the new variables
$({t,\xi })$ as
\begin{equation}\label{eq17}
\begin{gathered}
\frac{\partial }{\partial t}u({t,\xi })=u_t +uu_x =-P_x ({t,\xi }),\\
\frac{\partial }{\partial t}\eta ({t,\xi })=\eta _t +u\eta _x
=-({\eta +1})u_x ({t,\xi })
\end{gathered}
\end{equation}
From \eqref{eq9}, \eqref{eq11} and \eqref{eq4}, we obtain
\begin{equation}\label{eq18}
\begin{aligned}
\frac{\partial }{\partial t}\theta ({t,\xi })
&=\frac{2}{u_x \sqrt {u_x^2 -1} }({u_{xt} +uu_{xx} }) \\
&=-\csc \frac{\theta }{2}+({2u^2-2Au+\eta ^2+2\eta -2P})\cos
\frac{\theta }{2}\cdot \cot \frac{\theta }{2}.
\end{aligned}
\end{equation}
Furthermore, it follows from \eqref{eq9}, \eqref{eq11} and \eqref{eq6} that
\begin{equation} \label{eq19}
\frac{\partial }{\partial t}w({t,\xi })=({u_x^2 })_t +({uu_x^2 })_x
=({2u^2-2Au+\eta ^2+2\eta -2P})\cos \frac{\theta }{2}\cdot w.
\end{equation}
The functions $P$ and $P_x $ used in the above \eqref{eq17}-\eqref{eq19}
are given in \eqref{eq16}.

Now the corresponding Cauchy problems \eqref{eq17}-\eqref{eq19} for the
variables $({u,\eta ,\theta ,w})$ becomes the  semilinear system
\begin{equation} \label{eq20}
\begin{gathered}
 \frac{\partial u}{\partial t}=-P_x , \\
 \frac{\partial \eta }{\partial t}=-({\eta +1})\sec
\frac{\theta }{2}, \\
 \frac{\partial \theta }{\partial t}=-\csc \frac{\theta }{2}+(
{2u^2-2Au+\eta ^2+2\eta -2P})\cos \frac{\theta }{2}\cdot \cot
\frac{\theta }{2}, \\
 \frac{\partial w}{\partial t}=({2u^2-2Au+\eta ^2+2\eta -2P}
)\cos \frac{\theta }{2}\cdot w, \\
 \end{gathered}
\end{equation}
with the initial condition
\begin{equation} \label{eq21}
\begin{gathered}
 u({0,\xi })=\bar {u}({\bar {q}(\xi)}), \\
 \eta ({0,\xi })=\bar {\eta }({\bar {q}(\xi)}), \\
 \theta ({0,\xi })=2\operatorname{arcsec} \bar {u}_x ({\bar {q}(\xi)}), \\
 w({0,\xi })=1,
 \end{gathered}
\end{equation}
which can be regarded as an ordinary differential equation (ODE) in the
Banach space
\[
X=H^1\times [ {L^2\cap L^\infty } ]\times [ {L^2\cap
L^\infty } ]\times L^\infty ,
\]
endowed with the norm
\[
\| {({u,\eta ,\theta ,w})} \|_X =\| u
\|_{H^1} +\| \eta \|_{L^2} +\| \eta \|_{L^\infty
} +\| \theta \|_{L^2} +\| \theta \|_{L^\infty }
+\| w \|_{L^\infty } .
\]
In the dissipative case, we need modify the system \eqref{eq20} suitably.
Suppose that, along a given characteristic $t\to q({t,\xi })$, the wave
breaks at a first time $t=\tau (\xi)$.
As $t\uparrow \tau (\xi)$, the variable $\theta =2\operatorname{arcsec} u_x $
implies that $u_x ({t,\xi })\to -\infty $. For all $t\ge \tau $,
we set $\theta ({t,\xi })\equiv \pi $. Then the $P$ and $P_x $ in \eqref{eq16}
are replaced by
\begin{equation} \label{eq22}
\begin{aligned}
 P(\xi)&=\frac{1}{2}\int_{\{ {\theta ({{\xi }'}
)\ne \pi }\}} {\exp \Big\{ {-| {\int_{\{ {s\in
[ {\xi ,{\xi }'} ],\theta (s)\ne \pi } \}}
{\cos ^2\frac{\theta (s)}{2}\cdot w(s)ds} }
|} \Big\}} \\
&\quad \times ({u^2+\frac{1}{2}u_x^2 -Au+\frac{1}{2}\eta ^2+\eta }
) \cos ^2\frac{\theta }{2}\cdot w({{\xi }'})d{\xi }'
 \end{aligned}
\end{equation}
and
\begin{equation}\label{eq23}
\begin{aligned}
 P_x (\xi)
&=\frac{1}{2}\int_{\{ {{\xi }'>\xi
,\theta ({{\xi }'})\ne \pi } \}}
\exp\Big\{ {-| {\int_{\{ {s\in [ {\xi ,{\xi }'} ],\theta
(s)\ne \pi } \}} {\cos ^2\frac{\theta (s
)}{2}\cdot w(s)ds} } |} \Big\} \\
&\quad \times ({u^2+\frac{1}{2}u_x^2 -Au+\frac{1}{2}\eta ^2+\eta }
)\cdot \cos ^2\frac{\theta }{2}\cdot w({{\xi }'})d{\xi}' \\
&\quad -\frac{1}{2}\int_{\{ {{\xi
}'<\xi ,\theta ({{\xi }'})\ne \pi }\}}
\exp\Big\{ {-| {\int_{\{ {s\in [ {\xi ,{\xi }'} ],\theta
(s)\ne \pi } \}} {\cos ^2\frac{\theta (s
)}{2}\cdot w(s)ds} } |} \Big\} \\
&\quad \times ({u^2+\frac{1}{2}u_x^2 -Au+\frac{1}{2}\eta ^2+\eta }
)\cdot \cos ^2\frac{\theta }{2}\cdot w({{\xi }'})d{\xi}',
 \end{aligned}
\end{equation}
System \eqref{eq20} can thus be rewritten in the form
\begin{equation}\label{eq24}
\begin{gathered}
 \frac{\partial u}{\partial t}=-P_x ,
\\
 \frac{\partial \eta }{\partial t}=\begin{cases}
 -({\eta +1})\sec \frac{\theta }{2} &\text{if }\theta \ne \pi  \\
  0 &\text{if }\theta =\pi ,
 \end{cases}
 \\
 \frac{\partial \theta }{\partial t}=\begin{cases}
 -\csc \frac{\theta }{2}+({2u^2-2Au+\eta ^2+2\eta -2P})\cos
\frac{\theta }{2}\cdot \cot \frac{\theta }{2} &\text{if }\theta \ne \pi \\
  0 &\text{if }\theta =\pi,
 \end{cases}
 \\
 \frac{\partial w}{\partial t}=\begin{cases}
 ({2u^2-2Au+\eta ^2+2\eta -2P})\cos \frac{\theta }{2}\cdot
w &\text{if }\theta \ne \pi \\
0 &\text{if }\theta =\pi .
 \end{cases}
 \end{gathered}
\end{equation}
where the right hand side is now discontinuous. The discontinuity occurs
precisely when $\theta =\pi $.

\section{Global solutions of the equivalent semilinear system}

A unique local solution of the equivalent semilinear system defined on some
time interval $[0,T]$ is first obtained, and then it is
proved that this local solution can be globally extended for all times $t\ge
0$.
Denote
\begin{gather*}
U=({u,\eta ,\theta ,w})\in \mathbb{R}^4,
\\
F(U)=\begin{cases}
 \Big(0,\;-({\eta +1})\sec \frac{\theta }{2},\;
-\csc \frac{\theta}{2}+({2u^2-2Au+\eta ^2+2\eta })\cos \frac{\theta }{2}\\
\times \cot \frac{\theta }{2}, 
 ({2u^2-2Au+\eta ^2+2\eta })\cos \frac{\theta }{2}\cdot w\Big)
&\text{if }\theta \ne \pi ,\\[4pt]
 (0, 0, 0, 0) &\text{if } \theta =\pi ,
 \end{cases}
\\
G({\xi ,U(\cdot)})=\begin{cases}
 \Big(-P_x , 0,-2P\cos \frac{\theta }{2}\cdot \cot \frac{\theta }{2},-2P\cos
\frac{\theta }{2}\cdot w\Big)&\text{if }\theta \ne \pi , \\
 ({-P_x , 0, 0, 0})&\text{if } \theta =\pi .
 \end{cases}
\end{gather*}
The Cauchy problem for \eqref{eq24} is rewritten in more compact form with this
notation,
\begin{equation} \label{eq25}
\frac{\partial }{\partial t}U({t,\xi })=F({U({t,\xi})})+G({\xi ,U({t,\cdot })}),
\quad \xi \in \mathbb{R}
\end{equation}
with the initial condition
\[
U({0,\xi })=\bar {U}(\xi).
\]
After a solution $({u,\eta ,\theta ,w})$ of \eqref{eq25} is obtained,
a solution of \eqref{eq24} will be soon provided by the mapping
$({t,\xi })\to ({u,\eta ,\theta ,w})$. We regard \eqref{eq25} as an ODE
on the space $L^\infty (\mathbb{R},\mathbb{R}^4)$. Observe that the vector
field $F:R^4\to R^4$ is uniformly bounded and Lipschitz continuous as long
as $u,\eta $ remain in a bounded set. However, the nonlocal operator $G$ is
discontinuous.

To prove the unique local solution of the system \eqref{eq25}, we begin with some
assumptions.

\textbf{Assumption 1.} Suppose $F$ and $G$ are given in \eqref{eq25}, there exists
some constant $C>0$ and constant $\kappa ^\ast >0$ depending only on $C$
such that, for $U=({u,v,\theta ,w})\in L^\infty (\mathbb{R},\mathbb{R}^4)$,
$\tilde {U}=({\tilde {u},\tilde {v},\tilde {\theta },\tilde
{w}})\in L^\infty (\mathbb{R},\mathbb{R}^4)$, the following inequalities hold:
\begin{gather} \label{eq26}
\| u \|_{L^\infty } ,\| \eta \|_{L^\infty } ,\|
{\tilde {u}} \|_{L^\infty } ,\| {\tilde {\eta }}
\|_{L^\infty } \le C,
\quad
\frac{1}{C}\le w(\xi), \quad \tilde {w}(\xi)\le C,
\\
\label{eq27}
\operatorname{meas}({\{ {\xi ;\theta (\xi)\ne \pi ,| {\theta
(\xi)-\pi } |\ge \frac{\pi }{2}} \}}) \le C,
\\
\label{eq27b}
\operatorname{meas}({\{ {\xi ;\tilde {\theta }(\xi)\ne
\pi ,| {\tilde {\theta }(\xi)-\pi } |\ge \frac{\pi }{2}} \}})\le C,
\\
\label{eq28}
\| P \|_{L^\infty } +\| {P_x } \|_{L^\infty } \le \kappa ^\ast , \\
\label{eq28b}
\| P \|_{L^1} +\| {P_x } \|_{L^1} \le \kappa ^\ast
({1+\| u \|_{L^1} +\| \eta \|_{L^1} +\|
\theta \|_{L^1} }),
\\
\label{eq29}
\| {F(U)} \|_{L^\infty } ,\| {G(U)} \|_{L^\infty } \le \kappa ^\ast ,
\\
\label{eq30}
\| {F(U)-F({\tilde {U}})} \|_{L^\infty
} \le \kappa \| {U-\tilde {U}} \|_{L^\infty } ,
\\
\label{eq31}
\begin{aligned}
&\|{G(U)-G({\tilde {U}})} \|_{L^\infty}\\
&\le \kappa  \big[ {\| {U-\tilde {U}} \|_{L^\infty }
+\operatorname{meas}({\{ {\xi ;\theta \ne \pi ,\tilde {\theta }=\pi } \}}
)+\operatorname{meas}({\{ {\xi ;\tilde {\theta }\ne \pi ,\theta =\pi }
\}})} \big],
\end{aligned}
\end{gather}
where $\kappa $ is a Lipschitz constant.
\smallskip

\textbf{Assumption 2.}
Given initial data $\bar {z}=({\bar {u},\bar {\eta }})\in H^1\times L^2$,
there exists a constant $C>0$ such that
\[
\| u \|_{L^\infty } ,\| \eta \|_{L^\infty } \le \frac{C}{2},
\quad
\operatorname{meas}({\{ {\xi ;\theta (\xi)\ne \pi ,| {\theta
(\xi)-\pi } |\ge \frac{\pi }{4}} \}})\le
\frac{C}{2}.
\]
Define the set $\Omega ^\delta =\{ {\xi \in \mathbb{R};\bar {\theta }(\xi
)\in ({\pi ,\pi +\delta } ]\;} \}$, where
$\delta >0$ is a constant small enough. By possibly reducing the size of
 $\delta >0$, thus we can assume that
 $\operatorname{meas}({\Omega ^\delta })\le 1/(8\kappa )$.

Given $T>0$, let  $D$ be the set of all continuous mappings
$t\to U(t):[0,T]\to L^\infty ({R,R^4})$, with the following
properties:
\begin{gather*}
U(0)=\bar {U}, \\
\| {U(t)-U(s)} \|_{L^\infty } \le 2k^\ast | {t-s} |, \\
\theta ({t,\xi })-\theta ({t,\xi })\le -\frac{t-s}{2},
\quad \xi \in \Omega ^\delta ,\; 0\le s<t\le T.
\end{gather*}
Let  $\Pi :D\to D$ be defined by
\begin{equation}\label{eq32}
({\Pi (U)})({t,\xi })=\bar
{U}+\int_0^t {[ {F({U({\tau ,\xi })})+G(
{\xi ,U({\tau ,\cdot })})} ]} d\tau ,
\end{equation}
then a solution $t\to U(t)$ will be obtained as the unique
fixed point of the contractive transformation $\Pi :D\to D$.

With assumptions 1-2 and the definition of $D$, we are ready to prove the
existence and uniqueness of a local solution for Cauchy problem \eqref{eq25}.

\begin{theorem}\label{thm1}
Given $\bar {z}=({\bar {u}\;,\;\bar {\eta }} )\in H^1\times L^2$, the Cauchy
problem \eqref{eq25} has  a unique local solution defined
on a time interval $[0,T]$ with $T>0$ .
\end{theorem}

\begin{proof}
We first show that $\Pi :D\to D$ defined above is a strict contraction.
Choose $T>0$ sufficiently small and $U,\tilde {U}\in D$. Define
\begin{gather*}
\lambda =\mathop {\max }_{t\in [0,T]} \| {U(
t)-\tilde {U}(t)} \|_{L^\infty } ,
\quad
\tau (\xi)=\sup _{t\in [0,T]}
\{ {t;\theta ({t,\xi })\ne \pi } \},
\\
\tilde {\tau }(\xi)=\sup _{t\in [0,T]}
\{ {t;\tilde {\theta }({t,\xi })\ne \pi }\}
\end{gather*}
For each $\xi \in \Omega ^\delta $, we have
$| {\tau (\xi )-\tilde {\tau }(\xi)} |\le 2\lambda $. For
$t\in[0,T]$, we have
\begin{align*}
&\| {\Pi U(t)-\Pi \tilde {U}(t)}\|_{L^\infty }\\
&\le \int_0^t {\| {F({U(\tau)})-F(
 {\tilde {U}(\tau)})} \|_{L^\infty } d} \tau
 +\int_0^t {\| {G({U(\tau)})-G({\tilde
 {U}(\tau)})} \|_{L^\infty } d} \tau \\
&\le 2\kappa \int_0^t {\| {U(\tau)-\tilde {U}(\tau
)} \|_{L^\infty } d} \tau +\kappa \int_0^t {\operatorname{meas}({\{
{\xi ;\theta \ne \pi ,\tilde {\theta }=\pi } \}})d\tau }\\
&\quad +\kappa \int_0^t {\operatorname{meas}({\{ {\xi ;\tilde {\theta }
 \ne \pi ,\theta =\pi } \}})d\tau } \\
&\le 2T\kappa \lambda +\kappa \int_{\Omega ^\delta } {| {\tau (\xi
)-\tilde {\tau }(\xi)} |} d\xi \\
&\le 2\kappa T\lambda +2\kappa \operatorname{meas}({\Omega ^\delta }
) \lambda \le \frac{\lambda }{2},
\end{align*}
where $T$ is chosen as $T\le 1 /(8\kappa)$. This shows that $\Pi $ is
a strict contraction, which yields the desired local solution of Cauchy
problem \eqref{eq25}.

Next we  show that the local solutions of the semilinear system \eqref{eq24}
can be globally extended for all times $t\ge 0$.
In the following, we prove that the ``extended energy''
\[
\tilde {E}(t)=\int_R {\Big({u^2\cos ^2\frac{\theta _1
}{2}+\eta ^2\cos ^2\frac{\theta _1 }{2}+1}\Big)w} ({t,\xi }
)d\xi
\]
remains constant in time. We remark that the extended energy $\tilde
{E}(t)$ is strictly larger than the total energy
\[
E(t)=\int_{\{ {\theta ({t,\xi })\ne \pi }
\}} {\Big({u^2\cos ^2\frac{\theta }{2}+\eta ^2\cos ^2\frac{\theta
}{2}+1}\Big)w({t,\xi })} ({t,\xi })d\xi
\]
in the sense that here the integration ranges over the entire real line.

For future use, we show the following identities
\begin{equation}\label{eq33}
\begin{gathered}
u_\xi =u_x \cdot \frac{\partial y}{\partial \xi }=\sec \frac{\theta
}{2}\cdot \cos ^2\frac{\theta }{2}\cdot w=\cos \frac{\theta }{2}\cdot w,
\\
P_\xi =P_x \cdot \frac{\partial y}{\partial \xi }=P_x \cdot \cos
^2\frac{\theta }{2}\cdot w\,,
\end{gathered}
\end{equation}
hold for all times $t\ge 0$, as long as the solution is defined. Moreover,
when $\theta =\pi $, a separate computation yields
\[
u_\xi =0=\cos \frac{\pi }{2}\cdot w,
\quad
P_\xi =0=P_x \cdot \cos ^2\frac{\pi }{2}\cdot w.
\]
Thus the identity in \eqref{eq33} still holds for the cases
$\theta =\pi $. Then we obtain
\begin{gather*}
({uP})_\xi =u_\xi P+uP_\xi
=w({P\cdot \cos \frac{\theta }{2}+uP_x \cdot \cos ^2\frac{\theta }{2}}),\\
({u^3})_\xi =3u^2u_\xi =3wu^2\cdot \cos \frac{\theta }{2}, \\
({u^2})_\xi =2uu_\xi =2uw\cdot \cos \frac{\theta }{2}.
\end{gather*}
Differentiating the extended energy $\tilde {E}(t)$ with respect
to the variable $t$, we obtain
\begin{equation}
\label{eq34}
\begin{aligned}
&\frac{d}{dt}\int_R {\tilde {E}(t)} d\xi =\frac{d}{dt}\int_R
{\Big({u^2\cos ^2\frac{\theta }{2}+\eta ^2\cos ^2\frac{\theta }{2}+1}
\Big)w} d\xi \\
&=\int_R \Big[ \Big({u^2\cos ^2\frac{\theta }{2}+\eta ^2\cos ^2\frac{\theta
}{2}+1}\Big)\frac{\partial w}{\partial t}+\Big({2uu_t \cdot \cos
^2\frac{\theta }{2}-u^2\cos \frac{\theta }{2}\sin \frac{\theta
}{2}\frac{\partial \theta }{\partial t}}\Big)w
\\
&\quad +\Big({2\eta \eta _t \cdot \cos ^2\frac{\theta }{2}-\eta ^2\cos
\frac{\theta }{2}\sin \frac{\theta }{2}\frac{\partial \theta }{\partial t}}
\Big)w\Big]d\xi
\\
&=\int_{ \{\theta (\xi)\ne \pi  \}}
\Big\{2\Big({u^2\cos ^2\frac{\theta }{2}+\eta ^2\cos ^2\frac{\theta }{2}+1}\Big)
\Big({u^2-Au+\frac{\eta ^2}{2}+\eta -P}\Big)
\\
&\quad -2uP_x \cdot \cos \frac{\theta }{2}-2\eta ({\eta +1})-(
{u^2+\eta ^2})\sin \frac{\theta }{2}
\\
&\quad\times \big[ {-\csc \frac{\theta }{2}+({2u^2-2Au+\eta ^2+2\eta -2P}
)\cos \frac{\theta }{2}\cdot \cot \frac{\theta }{2}} \big]\Big\}\cos
\frac{\theta }{2} wd\xi
\\
&=\int_R {w\Big\{ {3u^2\cos \frac{\theta }{2}-2Au\cos \frac{\theta
}{2}-2P\cos \frac{\theta }{2}-2uP_x \cos ^2\frac{\theta }{2}} \Big\}} d\xi
\\
&=\int_R {\partial _\xi } ({u^3-Au^2-2uP})d\xi
=0.
\end{aligned}
\end{equation}
In the sense that $\cos \frac{\theta }{2}=0$ whenever $\theta =\pi $, thus
we are again integrating over the entire real line $R$ on the fourth
identity of \eqref{eq34}. This implies that the extended energy
$\tilde {E}(t)$ is consistent, namely
\begin{equation} \label{eq35}
\tilde {E}(t)=\int_R {\Big({u^2\cos ^2\frac{\theta _1
}{2}+\eta ^2\cos ^2\frac{\theta _1 }{2}+1}\Big)w} ({t,\xi }
)d\xi =\tilde {E}(0)=E_0 .
\end{equation}
From \eqref{eq33} and \eqref{eq35}, we can obtain the bound
\begin{equation}\label{eq36}
\sup _{\xi \in \mathbb{R}} | {u^2({t,\xi })}
|\le 2\int_R {| {uu_\xi } |} d\xi
\le 2\int_R {| u |\cdot | {\cos \frac{\theta }{2}} |}
wd\xi \le E_0 .
\end{equation}
This provides a priori bound on $\| {u(t)}
\|_{L^\infty } $, similarly we can derive an a priori bound on
$\| {\eta (t)} \|_{L^\infty } $. Also from the
estimation \eqref{eq35} and the definitions \eqref{eq21} and \eqref{eq22},
we obtain
\begin{equation}\label{eq37}
\begin{aligned}
&\| {P(t)} \|_{L^\infty } , \| {P_x (t)} \|_{L^\infty }\\
&\le \| G \|_{L^\infty }  \| {\big(
{u^2+\frac{1}{2}u_x^2 +\eta ^2}\big)(t)} \|_{L^1}
+\frac{A}{2}\big({\| G \|_{L^2}^2 +\| u \|_{L^2}^2 }\big)
+\frac{1}{2}\big({\| G \|_{L^2}^2 +\| \eta
\|_{L^2}^2 }\big)\\
&\le \frac{1}{2}E_0 +\frac{A}{2}({\frac{1}{4}+E_0 }
)+\frac{1}{2}({\frac{1}{4}+E_0 })\\
&\le \frac{2+A}{2}E_0 +\frac{A+1}{8}.
\end{aligned}
\end{equation}
Then by \eqref{eq36}, \eqref{eq37} and the fourth equation in \eqref{eq24},
we  deduce that there exists a constant $B$, depending only on the total
energy $E_0$, such that
\[
| {\frac{\partial w}{\partial t}} |\le Bw,
\]
which yields
\[
e^{-Bt}\le w(t)\le e^{Bt}.
\]
From the third equation in \eqref{eq24}, we know that
$0\le \theta (t)\le 2\pi$.

All the above estimates show that a priori bounds \eqref{eq26}-\eqref{eq28} which we
needed to construct a local solution with a constant $C$ exist over any
given time interval $[0,T]$. This completes the proof that
the local solution can be extended globally for all times $t\ge 0$.
\end{proof}

\section{Global dissipative solutions for the two-component Camassa-Holm
system}

In this section, we show that the global solution of the system \eqref{eq24}
yields a global dissipative solution of system \eqref{eq2}, in the original variables
$({t,x})$.
In the following, we shall show the continuous dependence of solutions to
system \eqref{eq2}. Recalling that we have obtained the local existence theorem by
representing the solution of \eqref{eq25} as the fixed point of a contraction in a
suitable space, this yields uniqueness and continuous dependence with
respect to convergence on the initial data in $L^\infty \times L^\infty $.

\begin{theorem}\label{thm2}
Let $\bar {z}_n =({\bar {u}_n ,\bar {\eta }_n })$ be a sequence of
 initial data with $\| {\bar {z}_n -\bar {z}} \|_{H^1}  \to 0$.
Then, for any T $>$ 0, the corresponding solutions
$z_n ({t,\xi })=({u_n ,\eta _n })({t,\xi })$ converge to
$z({t,\xi })=({u,\eta })({t,\xi })$ uniformly with $({t,\xi })\in [0,T]\times R$.
\end{theorem}

\begin{proof}
Let $({u,\eta ,\theta ,w})$ and $({\tilde {u},\tilde
{\eta },\tilde {\theta },\tilde {w}})$ be any two solutions of
\eqref{eq24}, with the initial condition \eqref{eq21}.
Let $E_0 $ be an upper bound for the energies of the two solutions.
 Suppose that at time $t=0$, there exists a constant $\delta _0 $,
\[
\| {z(0)-\tilde {z}(0)} \|_{L^\infty }
\le \delta _0 , \quad
\| {\theta ({0,\xi })-\tilde {\theta }({0,\xi }
)} \|_{L^2} \le \delta _0 .
\]
Next, for $t\in [0,T]$, we will establish an a-priori bound
depending only on $\delta _0 $, $T$ and $E_0 $ on
\begin{equation} \label{eq38}
\| {z(t)-\tilde {z}(t)} \|_{L^\infty }.
\end{equation}
Define the set
\[
\Lambda =\{ {\xi \in \mathbb{R};\theta ({T,\xi })=\pi }
\}\cup \{ {\xi \in \mathbb{R};\tilde {\theta }({T,\xi })=\pi
} \},
\]
thus $\alpha ^\ast =\operatorname{meas}(\Lambda)$ is a uniformly bounded
number depending only on $T$ and $E_0 $.

Let $\tau (\xi)=\inf \{ {t\in [0,T];\min\{ {\theta ({t,\xi }),
\tilde {\theta }({t,\xi } )} \}=\pi } \}$ such that $\tau (\xi)$ is the
first time when one of the two solutions reaches the value $\pi $. We now
construct a measure-preserving mapping:
$[ {0,\alpha ^\ast } ]\to \Lambda $, which is denoted as $\alpha \to \xi (\alpha)$
with the additional property:
\begin{equation} \label{e5.2}
\alpha \le {\alpha }' \text{ if and only if } \tau ({\xi (\alpha
)})\ge \tau ({\xi ({{\alpha }'})}).
\end{equation}
According to the mapping $[ {0,\alpha ^\ast } ]\to \Lambda $, we
define the distance function
\begin{equation}\label{eq39}
\begin{aligned}
&J({({u,\eta ,\theta ,w}),({\tilde {u},\tilde {\eta
},\tilde {\theta },\tilde {w}})}) \\
&=({\| {u-\tilde {u}} \|_{L^\infty } +\| {\eta -\tilde
{\eta }} \|_{L^\infty } +\| {\theta -\tilde {\theta }}
\|_{L^2} +\| {w-\tilde {w}} \|_{L^2} }) \\
&\quad +K_0 \int_0^{\alpha ^\ast } {e^{K\alpha }} ({| {\theta (
{\xi (\alpha)})-\tilde {\theta }({\xi (
\alpha)})} |})d\alpha .
\end{aligned}
\end{equation}
For convenience, we set
\begin{equation} \label{eq40}
J(t)=J({({u,v,\theta ,w}),({\tilde
{u},\tilde {v},\tilde {\theta },\tilde {w}})})(t
)=J^\ast (t)+K_0 J^\# (t),
\end{equation}
where
\[
J^\ast (t)=\Big({\| {u-\tilde {u}} \|_{L^\infty }
+\| {\eta -\tilde {\eta }} \|_{L^\infty } +\| {\theta
-\tilde {\theta }} \|_{L^2} +\| {w-\tilde {w}} \|_{L^2} }
\Big),
\]
\begin{equation} \label{eq41}
J^\# (t)=\int_0^{\alpha ^\ast } {e^{K\alpha }} \big({|
{\theta ({\xi (\alpha)})-\tilde {\theta }(
{\xi (\alpha)})} |}\big)d\alpha .
\end{equation}
In the following we  show that, for suitable constants $K_0 $, $K$, $M$
depending only on $T$ and $E_0 $, the inequality
\begin{equation}\label{eq42}
\frac{d}{dt}J(t)\le M J(t)
\end{equation}
holds. Moreover, this will imply
\[
J(t)\le e^{Mt}J(0), \quad t\in [0,T],
\]
which provides an a-priori estimate on the distance at \eqref{eq38}.

For each fixed $t\in [0,T]$, we define the sets
\begin{gather*}
\Gamma (t)=\{ {\xi \in \Lambda :\theta ({t,\xi }
)\ne \pi ,\tilde {\theta }({t,\xi })=\pi } \}\cup
\{ {\xi \in \Lambda :\tilde {\theta }({t,\xi })\ne \pi
,\theta ({t,\xi })=\pi } \},
\\
\Gamma ^+(t)=\{ {\xi \in \Lambda :\theta ({t,\xi }
)=\tilde {\theta }({t,\xi })=\pi } \},
\\
\Gamma ^-(t)=\{ {\xi \in \Lambda :\theta ({t,\xi }
),\tilde {\theta }({t,\xi })\ne \pi } \}=\{
{\xi \in \Lambda :\tau (t)>t} \},
\end{gather*}
with the following properties
\[
\Gamma (t)\cap \Gamma ^+(t)=\Gamma (t
)\cap \Gamma ^-(t)=\Gamma ^+(t)\cap \Gamma ^-(t)=\Phi ,
\quad
\Gamma (t)\cup \Gamma ^+(t)\cup \Gamma ^-(t)=\Lambda
\]
for each $t\in [0,T]$.
Set $m(t)=\operatorname{meas}({\Gamma ^-(t)})$, such
that
\begin{equation}\label{eq43}
\Gamma ^-(t)=\{ {\xi (\alpha);\alpha \in
[ {0,m(t)} ]} \}.
\end{equation}
From the equations in \eqref{eq24}, we have the  estimate
\begin{equation}\label{eq44}
\begin{aligned}
&\frac{d}{dt}\Big({\| {u-\tilde {u}} \|_{L^\infty } +\|
{\eta -\tilde {\eta }} \|_{L^\infty } +\| {\theta -\tilde {\theta
}} \|_{L^2} +\| {w-\tilde {w}} \|_{L^2} }\Big)
\\
&\le \kappa \Big({\| {u-\tilde {u}} \|_{L^\infty } +\|
{\eta -\tilde {\eta }} \|_{L^\infty } +\| {\theta -\tilde {\theta
}} \|_{L^2} +\| {w-\tilde {w}} \|_{L^2} +\operatorname{meas}({\Gamma
(t)})}\Big).
\end{aligned}
\end{equation}
Moreover, from \eqref{eq43} we can deduce that
\begin{equation} \label{eq45}
\begin{aligned}
&\frac{d}{dt}\int_0^{\alpha ^\ast } {e^{K\alpha }({| {\theta
({t,\xi (\alpha)})-\tilde {\theta }({t,\xi
(\alpha)})} |})} d\alpha \\
&=\int_{\Gamma (t)\cup \Gamma ^+(t)\cup \Gamma
^-(t)} {e^{K\alpha (\xi)}\cdot \frac{\partial
}{\partial t}({| {\theta ({t,\xi (\alpha)}
)-\tilde {\theta }({t,\xi (\alpha)})}
|})} d\alpha \\
&=\int_{\Gamma (t)} {e^{K\alpha (\xi)}\cdot
\frac{\partial }{\partial t}({| {\theta ({t,\xi (
\alpha)})-\tilde {\theta }({t,\xi (\alpha)}
)} |})} d\xi
\\
&\quad +\int_0^{m(t)} {e^{K\alpha (\xi)}\cdot
\frac{\partial }{\partial t}({| {\theta ({t,\xi (
\alpha)})-\tilde {\theta }({t,\xi (\alpha)}
)} |})} d\alpha .
\end{aligned}
\end{equation}
Indeed, the integral over $\Gamma ^+(t)$ is zero.

Choosing $\delta >0$ which depends only on $T$, $E_0 $ sufficiently small,
we have
\[
| {\theta ({t,\xi })-\tilde {\theta }({t,\xi })} |\le \delta
\]
for $\xi \in \Gamma (t)$, which implies
\[
\frac{\partial }{\partial t}| {\theta ({t,\xi })-\tilde
{\theta }({t,\xi })} |\le -\frac{1}{2}.
\]
On the other hand, choosing a constant $\kappa $ large enough such that
$| {\theta ({t,\xi })-\tilde {\theta }({t,\xi })} |\ge \delta $, we obtain
\[
\frac{\partial }{\partial t}| {\theta ({t,\xi })-\tilde
{\theta }({t,\xi })} |\le -\frac{1}{2}+\kappa |
{\theta ({t,\xi })-\tilde {\theta }({t,\xi })}|.
\]
Finally, for $\xi \in \Gamma ^-(t)$, we have
\begin{align*}
\frac{\partial }{\partial t}| {\theta ({t,\xi })-\tilde
{\theta }({t,\xi })} |
&\le \kappa \cdot (\| {u-\tilde
{u}} \|_{L^\infty } +\| {\eta -\tilde {\eta }} \|_{L^\infty
} +\| {\theta -\tilde {\theta }} \|_{L^2} +\| {w-\tilde {w}}
\|_{L^2}\\
&\quad +\operatorname{meas}({\Gamma (t)})+| {\theta ({t,\xi }
)-\tilde {\theta }({t,\xi })} |).
\end{align*}
Therefore,
\begin{equation}\label{eq46}
\begin{aligned}
&\int_0^{m(t)} {e^{K\alpha }\cdot \frac{\partial }{\partial
t}({| {\theta ({t,\xi (\alpha)})-\tilde
{\theta }({t,\xi (\alpha)})} |})} d\alpha \\
& \le \kappa ({J^\ast (t)+\operatorname{meas}({\Gamma (t
)})})\int_0^{m(t)} {e^{K\alpha }d\alpha }
+\kappa \int_0^{m(t)} {e^{K\alpha }\Big({| {\theta
({t,\xi (\alpha)})-\tilde {\theta }({t,\xi
(\alpha)})} |}\Big)d\alpha }
\\
&\le \kappa ({J^\ast (t)+\operatorname{meas}({\Gamma (t
)})})\int_0^{m(t)} {e^{K\alpha }d\alpha }
+\kappa \int_{\Gamma ^-(t)} {e^{K\alpha (\xi
)}\big({| {\theta ({t,\xi })-\tilde {\theta
}({t,\xi })} |}\big)} d\xi .
\end{aligned}
\end{equation}
Now, \eqref{eq44} can be rewritten in the  form
\begin{equation}\label{eq47}
\frac{d}{dt}J^\ast (t)\le \kappa \cdot ({J^\ast (t
)+\operatorname{meas}({\Gamma (t)})}).
\end{equation}
Notice that $\xi \in \Gamma (t)$ implies $\alpha (\xi)\ge m(t)$,
together \eqref{eq45} and \eqref{eq46} imply
\begin{equation}\label{eq48}
\begin{aligned}
\frac{d}{dt}J^\# (t)
&\le -\frac{1}{2}\int_{\Gamma (t)} {e^{K\alpha (\xi)}} d\xi
+\kappa \int_{\Gamma (t)\cup \Gamma ^-(t)} {e^{K\alpha (\xi)}(
{| {\theta ({t,\xi })-\tilde {\theta }({t,\xi })} |})} d\xi \\
&\quad +\kappa  ({J^\ast (t)+\operatorname{meas}({\Gamma (t
)})})\cdot \int_0^{m(t)} {e^{K\alpha}d\alpha } \\
&\le -\frac{1}{2}e^{Km(t)} \operatorname{meas}({\Gamma (t
)})+\kappa J^\# (t)+\kappa J^\ast (t)\int_0^{\alpha ^\ast }
{e^{K\alpha }d\alpha } \\
&\quad +\kappa  \operatorname{meas}({\Gamma (t)})e^{Km(t
)}\int_0^{m(t)} {e^{K({\alpha -m(t)} )}d\alpha } \\
& \le -\frac{1}{4}e^{Km(t)}\operatorname{meas}({\Gamma (t
)})+\kappa J^\# (t)+\frac{\kappa }{K}e^{K\alpha^\ast }J^\ast (t).
\end{aligned}
\end{equation}
We choose the constant $K=4\kappa $ in the above inequality such that
\[
\kappa \int_0^{m(t)} {e^{K({\alpha -m(t)}
)}d\alpha } \le \frac{\kappa }{K}=\frac{1}{4}.
\]
From \eqref{eq47} and \eqref{eq48}, choosing $K_0 =4k$, we obtain
\begin{align*}
&\frac{d}{dt}({J^\ast (t)+4\kappa J^\# (t)})\\
&\le \kappa \cdot ({J^\ast (t)+\operatorname{meas}({\Gamma(t)})})
+4\kappa ({-\frac{1}{4}\operatorname{meas}({\Gamma (t)}
)+\kappa J^\# (t)+\frac{\kappa }{K}e^{K\alpha ^\ast
}J^\ast (t)}) \\
&\le \kappa J^\ast (t)+4\kappa ^2J^\# (t)+\kappa
e^{4\kappa \alpha ^\ast }J^\ast (t),
\end{align*}
with $J^\ast $ and $J^\# $ are defined in \eqref{eq41}.
With $M=\kappa +\kappa e^{4\kappa \alpha ^\ast }$, our
claim \eqref{eq42} is satisfied.
\end{proof}

Next we  revert to the original variables
$({t,x})$, and show that the global solution of system \eqref{eq24}
yields a global dissipative solution of the original system \eqref{eq2}.

Let us begin with a global solution $({u,\eta ,\theta ,w})$ of
system \eqref{eq24}. Define
\begin{equation}\label{eq49}
q({t,\xi })=\bar {q}(\xi)+\int_0^t {u({\tau,\xi })d\tau } .
\end{equation}
Then for each fixed $\xi $, the function $t\mapsto q({t,\xi })$
provides a solution to the Cauchy problem
\begin{equation}\label{eq50}
\begin{gathered}
 \frac{\partial }{\partial t}q({t,\xi })=u({t,\xi }), \\
 q({0,\xi })=\bar {q}(\xi).
 \end{gathered}
\end{equation}
We claim that, if $q({t,\xi })=x$, a solution of system \eqref{eq2}
can be obtained by setting
\begin{equation}\label{eq51}
z({t,x})=z({t,\xi }),
\end{equation}
where $z({t,x})=({u,\;\eta })({t,x})$,
$z({t,\xi })=({u,\;\eta })({t,\xi})$.
The main result reads as follows.

\begin{theorem}\label{thm3}
 If  $({u,\eta ,\theta ,w})$ is a global
solution to the Cauchy problem \eqref{eq24}-\eqref{eq21}, then the function
$z=z({t,x})$ defined by \eqref{eq48}-\eqref{eq51} provides a global
dissipative solution of system \eqref{eq2}.
\end{theorem}

\begin{proof}
Using the uniform bound $| {u({t,\xi })}|\le E_0^{1/2}$,
  from \eqref{eq48} we obtain
\[
\bar {q}(\xi)-E_0^{1/ 2} t\le q({t,\xi })\le \bar
{q}(\xi)+E_0^{1/2} t, \quad t\ge 0.
\]
The definition of $\xi $ in \eqref{eq10} yields
\[
\lim _{\xi \to \pm \infty } \bar {q}({t,\xi })=\pm \infty .
\]
Then the image of the continuous map
$({t,\xi })\to ({t,q({t,\xi })})$ covers the entire plane
$[{0,\infty } ]\times R$. It is clear that the map
$\xi \mapsto q({t,\xi })$ is non-decreasing. Then the map
$({t,x})\mapsto z({t,x})$ at \eqref{eq51} is well defined, for all
$t\ge 0$ and $x\in \mathbb{R}$.

For every fixed $t$, we claim
\begin{align*}
\operatorname{meas}({\{ {q({t,\xi });\theta ({t,\xi })=\pi } \}})
&=\int_{\{ {\theta ({t,\xi })=\pi } \}} {q_\xi ({t,\xi })d\xi }\\
&=\int_{\{ {\theta ({t,\xi })=\pi } \}} {w\cos ^2\frac{\theta }{2}({t,\xi })d\xi } 
=0,
\end{align*}
which implies that, in the $x$-variable, the image of the singular set, where
$\theta =\pi $, has measure zero.

By changing the variable of integration, we compute
\begin{equation}\label{eq52}
\begin{aligned}
&\int_R {({u^2+u_x^2 +\eta ^2})({t,x})} dx \\
&=\int_{\{ {\cos \theta \ne -1} \}} {({u^2\cos
^2\frac{\theta }{2}+\eta ^2\cos ^2\frac{\theta }{2}+1})}
 w({t,\xi })d\xi \le E_0 .
\end{aligned}
\end{equation}
This implies the uniform H\"{o}lder continuity with exponent
$1/ 2$ of $z$ as a function of $x$. From the first and second equations
in \eqref{eq24} and the bounds on $\| P \|_{L^\infty } $,
$\| {P_x } \|_{L^\infty } $, we can obtain that the map
$t\mapsto z({t,q(t)})$ is uniformly Lipschitz continuous along the
characteristic curve $t\mapsto q(t)$. Hence, $z=z({t,x})$ is globally
 H\"{o}lder continuous for $({t,x})\in \mathbb{R}^+\times \mathbb{R}$.

We know that the map $t\to z(t)$ is Lipschitz continuous with
values in $L^2(\mathbb{R})$. Since $L^2(\mathbb{R})$ is a reflexive
space, we can deduce that the map $t\mapsto q(t)$ is
differentiable for almost every (a.e.) time $t\ge 0$. Note that the right
hand side of the first equation in \eqref{eq8} lies in $L^2(\mathbb{R})$, to
establish the equality, one may proceed as follows.

For each smooth function with compact support $\varphi \in C_c^\infty $, at
a. e. time $t\ge 0$, we have
\begin{equation} \label{eq53}
\begin{aligned}
&\frac{d}{dt}\int {u({t,x})\varphi (x)} dx
=\int {({-uu_x -P_x })({t,x})\varphi (x)}dx \\
&=\int {[ {u^2({t,x}){\varphi }'(x)-P_x (
{t,x})\varphi (x)+u({t,x})u_x ({t,x})\varphi (x)} ]} dx.
\end{aligned}
\end{equation}
Let us set
\begin{equation}\label{eq54}
\tau (\xi)=\inf \{ {t>0;\theta (t)=\pi }\}
\end{equation}
for each $\xi \in \mathbb{R}$. Note that, for a. e. time $t\ge 0$
\begin{equation}\label{eq55}
\operatorname{meas}({\{ {\xi ;\tau (\xi)=t} \}})=0.
\end{equation}
Choosing a time $t$ such that \eqref{eq55} holds.
Integrating with respect to the variable $\xi $ and thus we obtain
from \eqref{eq13} that
\begin{align*}
&\frac{d}{dt}\int {u({t,\xi })\varphi ({q({t,\xi }
)})({w\cdot \cos ^2\frac{\theta }{2}})} ({t,\xi })d\xi \\
&=\int \big\{ {u_t \varphi w\cos ^2\frac{\theta }{2}
+u{\varphi }'q_t w\cos ^2\frac{\theta }{2}+u\varphi w_t
\cos ^2\frac{\theta }{2}-u\varphi w\theta
_t \frac{\sin \theta }{2}} \big\} d\xi \\
&=\int_{\theta ({t,\xi })\ne \pi }
 \Big\{ {-P_x \varphi w\cos ^2\frac{\theta }{2}}
 +u^2{\varphi }'w\cos ^2\frac{\theta}{2}
 +u\varphi  ({2u^2-2Au+\eta ^2+2\eta -2P}) \\
&\quad\times \cos \frac{\theta}{2}w  \cos ^2\frac{\theta }{2}
 -u\varphi w\big[ -\csc \frac{\theta}{2} +({2u^2-2Au+\eta ^2+2\eta -2P})\\
&\quad \cos \frac{\theta }{2}\cot \frac{\theta }{2} \big]
 \frac{\sin \theta }{2} \Big\} d\xi \\
&=\int_{\theta ({t,\xi })\ne \pi } {[ {-P_x \varphi
+u^2{\varphi }'+uu_x \varphi } ]} w\cos ^2\frac{\theta }{2}d\xi .
\end{align*}
It can be seen \eqref{eq53} holds, and therefore we can conclude that
$z=({u,\eta })$ is a global solution of the two-component Camassa-Holm
system in the sense of Definitions \ref{def1} and \ref{def2}.
\end{proof}

Next we  prove that global dissipative solutions of the two-component
Camassa-Holm system \eqref{eq2} construct a semigroup.
To do this some relevant properties are first given.
\smallskip

\textbf{Property 1.}
The total energy is a non-increasing function of time, namely
$\| {z(t)} \|_{H^1(\mathbb{R})} \le \|{z({{t}'})} \|_{H^1(\mathbb{R})} $
if $0\le {t}'\le t$.

\begin{proof}
By \eqref{eq52}, we have
\begin{align*}
\| {z(t)} \|_{H^1}
&=\int_R {({u^2+u_x^2 +\eta ^2})({t,x})} dx \\
&=\int_{\{ {\cos \theta \ne -1} \}} \Big({u^2\cos
^2\frac{\theta }{2}+\eta ^2\cos ^2\frac{\theta }{2}+1}\Big) w({t,\xi })d\xi \\
&=E_0 -\int_{\{ {\tau (\xi)\le t} \}} \Big(
{u^2\cos ^2\frac{\theta }{2}+\eta ^2\cos ^2\frac{\theta }{2}+1}\Big)
w({t,\xi })d\xi \\
&\le E_0 -\int_{\{ {\tau (\xi)\le t} \}} {w({t,\xi })} d\xi\\
&\le E_0 -\int_{\{ {\tau (\xi)\le {t}'} \}} {w({t,\xi })} d\xi
=\| {z({{t}'})} \|_{H^1}
\end{align*}
with $\tau (\xi )$ given in \eqref{eq54}.
\end{proof}

\textbf{Property 2.}
Given a sequence of initial data $\bar {z}_n $
such that $\bar {z}_n \to \bar {z}$ in $H^1\times L^2$, the corresponding
solutions $z_n ({t,x})\to z({t,x})$ uniformly for
$({t,x})$ in bounded sets.

\begin{theorem}\label{thm4}
Let  $\bar {z}_n \in H^1\times [ {L^2\cap L^\infty } ]$ be an initial data,
and $z(t)=S_t \bar {z}$ the corresponding global solution of system
\eqref{eq2} constructed in Theorem \ref{thm3}.
Then the mapping S: $H^1\times [ {L^2\cap L^\infty }]\times [ {0,\infty })\to H^1$
is a semigroup.
\end{theorem}

\begin{proof}
Let $({t,\xi })\to ({u,\eta ,\theta ,w})({t,\xi })$ be the corresponding
solutions to systems \eqref{eq24} and \eqref{eq21}. For the fixed
$\tau >0$ and all $t\in \mathbb{R}^+$, one needs to prove that
\[
S_t ({S_\tau \bar {z}})=S_{\tau +t} \bar {z}.
\]
A new energy variable $p$ is defined as
\begin{equation}\label{eq56}
\frac{d}{d\xi }p(\xi)=\begin{cases}
 w({\tau ,\xi })&\text{if }\theta ({\tau ,\xi })\ne \pi , \\
 0&\text{if } \theta ({\tau ,\xi })=\pi ,
 \end{cases}
\end{equation}
with initial data
\begin{equation}\label{eq57}
p({\xi _0 })=0.
\end{equation}
Choose the value $\xi _0 $ such that $q({\tau ,\xi _0 })=0$. By
setting $\hat {z}=S_\tau \bar {z}$, we define
\begin{equation}\label{eq58}
\begin{gathered}
 \hat {z}({t,p})=z({\tau +t,\xi (p)}), \\
 \hat {\theta }({t,p})=\theta ({\tau +t,\xi (p)}), \\
 \hat {w}({t,p})=\frac{w({\tau +t,\xi (p)})}{w({\tau ,\xi (p)})}, \\
 \end{gathered}
\end{equation}
such that $p\to \xi (p)$ provides an a.e. inverse to the
mapping in \eqref{eq56}-\eqref{eq57}, namely,
\[
\xi ({p^\ast })=\sup \{ {s;p(s)\le p^\ast }\}.
\]
Recalling the identities \eqref{eq14} and \eqref{eq13}, one has
\[
\frac{\partial }{\partial \xi }q({\tau ,\xi })\cdot u_x^2
({\tau ,q({\tau ,p(\xi)})})
=w({\tau ,\xi })=\frac{d}{d\xi }p(\xi).
\]
By an integration and using \eqref{eq56}, one gets that
\[
\int_0^{q({\tau ,\xi })} {u_x^2 ({\tau ,x})}dx=p(\xi).
\]
Now it can be shown that the functions in \eqref{eq58} provide
a solution to system \eqref{eq24}. The identities
$w({\tau +t,\xi })d\xi =\frac{\hat {w}({t,p(\xi)})}{w({t,p(
\xi)})}\cdot \frac{dp(\xi)}{d\xi }\cdot dp=\hat
{w}({t,p(\xi)})dp$ imply that the corresponding
integral source terms in \eqref{eq24} satisfy
\begin{equation}\label{eq59}
\hat {P}({t,p})=P({\tau +t,\xi (p)}),\quad
\hat {P}_x ({t,p})=P_x ({\tau +t,\xi (p)}).
\end{equation}
Since the last equation in \eqref{eq24} is linear with respect to the variable
$w$, then we can draw the conclusion that the functions in \eqref{eq58} provide a
solution to system \eqref{eq24}. In summary, the global dissipative solutions of
system \eqref{eq2} construct a semigroup.
\end{proof}

\subsection*{Acknowledgements}
 This work was supported in part by the Major State Basic Research 
Development Program 973 (No. 2012CB215202), and by the National Natural 
Science Foundation of China (No.61134001). 

\begin{thebibliography}{00}

\bibitem{a1} N. Aronszajn;
\emph{Differentiability of Lipschitzian mappings between Banach spaces},
Studia Math.57 (1976), 147--190.

\bibitem{b1} A. Bressan, A. Constantin;
\emph{Global conservative solutions of the Camassa--Holm equation},
 Arch. Ration. Mech. Anal. 183 (2007), 215--239.

\bibitem{b2} A. Bressan, A. Constantin;
\emph{Global dissipative solutions of the Camassa--Holm equation},
 Appl. Anal. 5 (2007), 1--27.

\bibitem{c1} R. Camassa, D. Holm;
\emph{An integrable shallow water equation with peaked solitons},
Phys. Rev. Lett. 71 (1993), 1661--1664.

\bibitem{c2} M. Chen, S.-Q. Liu, Y. Zhang;
\emph{A 2-component generalization of the Camassa--Holm equation and its solutions},
Lett. Math. Phys. 75 (2006), 1--15.


\bibitem{c3} A. Constantin;
\emph{The Hamiltonian structure of the Camassa--Holm equation},
Expo. Math.15 (1997), 53--85.

\bibitem{c4} A. Constantin;
\emph{On the scattering problem for the Camassa--Holm equation},
Proc. R. Soc. Lond. Ser. A Math. Phys. Eng. Sci. 457 (2001), 953--970.

\bibitem{c5} A. Constantin;
\emph{Global existence of solutions and breaking waves for a shallow water
equation: a geometric approach}, Ann. Inst. Fourier (Grenoble) 50 (2000),
 321--362.

\bibitem{c6} A. Constantin, J. Escher;
\emph{Wave breaking for nonlinear nonlocal shallow water equations},
 Acta Math.181 (1998), 229--243.

\bibitem{c7} A. Constantin, R. Ivanov;
\emph{On an integrable two-component Camassa--Holm shallow water system},
Phys. Lett. A 372 (2008), 7129--7132.

\bibitem{c8} A. Constantin, D. Lannes;
\emph{The hydrodynamical relevance of the Camassa-Holm and Degasperis-Procesi
equations}, Arch. Ration. Mech. Anal. 192 (2009), 165--186.

\bibitem{e1} J. Escher, O. Lechtenfeld,  Z.Y. Yin;
\emph{Well-posedness and blow-up phenomena for the 2-component Camassa-Holm equation},
 Discrete Contin. Dyn. Syst. 19 (2007), 493--513.

\bibitem{f1} G. Falqui;
\emph{On a Camassa--Holm type equation with two dependent variables},
J. Phys. A 39 (2006), 327--342.

\bibitem{g1} C. Guan, Z. Y. Yin;
\emph{Global existence and blow-up phenomena for an integrable two-component
 Camassa-Holm shallow water system}, J. Diff. Eq. 248 (2010), 2003--2014.

\bibitem{g2} G. Gui, Y. Liu;
\emph{On the Cauchy problem for the two-component Camassa-Holm system},
 Math. Z. 268 (2011), 45--66.

\bibitem{g3} G. Gui, Y. Liu;
\emph{On the global existence and wave-breaking criteria for the two-component
Camassa-Holm system}, J. Funct. Anal. 258 (2010), 4251--4278.

\bibitem{h1} D. D. Holm, C. Tronci;
\emph{Geodesic ows on semidirect-product Lie groups: geometry of singular
measure-valued solutions}. Proc. R. Soc. London Ser. A 465 (2009), 457--476.

\bibitem{j1} R. S. Johnson;
\emph{Camassa--Holm, Korteweg--de Vries and related models for water waves},
J. Fluid Mech. 455 (2002),  63--82.

\bibitem{o1} P. Olver, P. Rosenau;
\emph{Tri-Hamiltonian duality between solitons and solitary-wave solutions
 having compact support},  Phys. Rev. E (3) 53 (1996), no. 2, 1900--1906.


\bibitem{t1} L. Tian, Y. Wang;
\emph{Global conservative and dissipative solutions of a coupled Camassa-Holm
equations}, J. Math. Phys. 52 (2011), 063702, 29 pp.

\bibitem{w1} Y. Wang, J. Huang;
\emph{Global conservative solutions of the two-component Camassa-Holm shallow
water system}, Int. J. Nonlinear Sci. 9 (2010), 379--384.

\bibitem{w2} Y. Wang, Y. D. Song;
\emph{Global conservative and multipeakon conservative solutions for the
two-component Camassa-Holm system}, Boundary Value Problems
DOI:10.1186/1687-2770-2013-165.

\bibitem{w3} Y. Wang, Y. D. Song;
\emph{Dissipative solutions for the modified two-component Camassa-Holm system},
Nonlinear Differ. Equ. Appl. DOI: 10.1007/s00030-013-0249-7.

\end{thebibliography}

\end{document}
