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This is the abstract of the test branch version. Another change to see how I can see differences between files.  }
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{Stephan R. de Roode\thanks{Corresponding author address:  Stephan R. de Roode, s.r.deroode@tudelft.nl, Department of Geoscience and Remote Sensing, Delft University of Technology, Delft, The Netherlands.} ,
 Author 2\thanks{\textit{The Beach}}
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\section{Introduction}
Stratocumulus 
   

\subsection{Summary }

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\begin{figure*}[ht]
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\begin{table*}
\begin{tabular}{ l l l l l l}
\hline
     &          & ASTEX & Fast & Reference & Slow \\           
\hline 
latitude  & $^0$N  &     34 &   25  &   25 & 25  \\
longitude & $^0$W  &     25 &   125  &   125 & 125  \\
date      &        & 13 June  & 15 July & 15 July & 15 July \\ 
Div       & 10$^{-6}$ s$^{-1}$   &  - & 1.9 & 1.86 & 1.84 \\  
z$_{\mathrm{Div}}$ & km & 1.6 & 2  & 2 & 2 \\
\hline       
\end{tabular}   
\caption{Details of the simulations. Div represents the large-scale divergence of the horizontal mean wind velocities, which is constant in time and constant up to a height of z$_{\mathrm{Div}}$, except for the ASTEX case in which the divergence varies with time.}
\label{tab:set_up}
\end{table*}
 
\begin{acknowledgment}
The investigations were done  
\end{acknowledgment}


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\begin{appendices}

\section{A mixed-layer model for the subcloud layer}

The budget equation for 
\end{appendices}

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