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\newcommand{\titelname}{Reconstruct Past Climate\\{\small Data Source, Proxies}}

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\date{Large-scale climate variability, 13.11.2006}
\author{Thomas Kuster\\ {\small \hyperref{http://fam-kuster.ch/index.php?navigation=ETH&main=http://n.ethz.ch/student/kusterth/eth/html/}{}{}{http://fam-kuster.ch}}}
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\section{Parameter and Resolution}
The follow-up weather parameters normaly could reconstruct:
\begin{itemize}
\item temperature
\item precipitation
\item wind
\end{itemize}
The Resolution depends on the data source. % and can go from more then daily to less then annual.

\section{Data Source}
Descriptive documentary data such as:
\begin{itemize}
\item reports from chronicles
\item daily weather reports
\item travel diaries
\item ship logbooks
\end{itemize}

Documentary proxy data are more indirect evidence that reflects weather or climate conditions.

\subsection{Speleothem}
Speleothems are secondary cave deposits such as stalactites and stalagmites (Stala{\bf g}mites grow from the {\bf g}round, stala{\bf c}tites grow from the {\bf c}eiling).

\subsubsection{Development of Speleothems}
\begin{tabular}{rcl}
CaCO$_3$ + H$_2$O + CO$_2$ & $\Longrightarrow$ & Ca$_2^+$ + 2 HCO$_3^-$\\
Ca$_2^+$ + 2 HCO$_3^-$ & $\Longrightarrow$ & CaCO$_3$ + H$_2$O + CO$_2$
\end{tabular}

\subsubsection{Age}
Thorium-Uran method

\subsubsection{Precipitation}
The $\delta^{18}$O depends on the precipitation. The $\delta^{18}$O is more negativ in periods with more precipitation.

%\subsubsection[Comparison of the Stalagmite d18O Record with the d18O Ice Core Record]{Comparison of the Stalagmite $\delta^{18}$O Record with the $\delta^{18}$O Ice Core Record}
\includegraphics[page=2,clip,viewport=222 394 571 564, width=\linewidth]{./password/fleitmann2003}

\section{Discussion}
\begin{itemize}
\item Different proxies and their pros and cons
\item The $\delta^{18}$O dependence on precipitation
\end{itemize}

\begin{thebibliography}{10}
\bibitem{lionello}
 P.~Lionello et.\,al.
 \newblock The Mediterranean Climate: An Overview of the Main Characteristics and Issues.
 \newblock {\em Developments in Earth \& Environmental Sciences}, 4:27--148, 2006.
  
\bibitem{fleitmann}
 D.~Fleitmann et.\,al.
 \newblock Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman.
 \newblock {\em Science}, 300:1737--1739, 2003.
\end{thebibliography}

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