
% Figure 1 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.5\textwidth]{Fig1}
  \caption{Topographic height over the domain used for diagnostics (m).}\label{Fig1}
\end{figure}

% Figure 2 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig2}
  \caption{Climatological mean (top row), climatological intraseasonal standard deviation (middle row) and interannual seasonal standard deviation (bottom row) of precipitation ($1^{st}$ column), evapotranspiration ($2^{nd}$ column), vertically integrated atmospheric water flux divergence ($3^{rd}$ column) and vertically integrated water vapour tendency ($4^{th}$ column), calculated from the CRCM simulation for the winter season from December 1960 to February 1990. Units are in mm/day.}\label{Fig2}
\end{figure}

% Figure 3 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig3}
  \caption{Climatological intraseasonal variance of the total (top row), large-scale component (middle row) and small-scale component plus covariance (bottom row) of precipitation ($1^{st}$ column), evapotranspiration ($2^{nd}$ column), vertically integrated atmospheric water flux divergence ($3^{rd}$ column) and vertically integrated water vapour tendency ($4^{th}$ column), calculated from the CRCM simulation for the winter season from December 1960 to February 1990. Units are in mm$^2$/day$^2$.}\label{Fig3}
\end{figure}

% Figure 4 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.5\textwidth]{Fig4}
  \caption{Climatological intraseasonal variance ($1^{st}$ column) and interannual seasonal variance ($2^{nd}$ column) of the total vertically integrated atmospheric water flux divergence (top row), its CGCM3-resolved contribution (middle row), and its CGCM3-unresolved contribution plus covariance (bottom row), calculated on pressure levels from the CRCM simulation for the winter season from December 1960 to February 1990. Units are in mm$^2$/day$^2$.}\label{Fig4}
\end{figure}

% Figure 5 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.75\textwidth]{Fig5}
  \caption{Climatological intraseasonal standard deviation of the nine interaction terms entering the vertically integrated atmospheric water flux divergence, calculated on pressure levels from the CRCM simulation for the winter season from December 1960 to February 1990. Units are in mm/day.}\label{Fig5}
\end{figure}

% Figure 6 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig6}
  \caption{Same as \ref{Fig2} but for the summer season from June 1961 to August 1990.}\label{Fig6}
\end{figure}

% Figure 7 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig7}
  \caption{Same as \ref{Fig3} but for the summer season from June 1961 to August 1990.}\label{Fig7}
\end{figure}

% Figure 8 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.5\textwidth]{Fig8}
  \caption{Same as \ref{Fig4} but for the summer season from June 1961 to August 1990.}\label{Fig8}
\end{figure}

% Figure 9 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.75\textwidth]{Fig9}
  \caption{Same as \ref{Fig5} but for the summer season from June 1961 to August 1990.}\label{Fig9}
\end{figure}

% Figure 10 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig10}
  \caption{Changes in the climatological mean of precipitation ($1^{st}$ panel), evapotranspiration ($2^{nd}$ panel) and vertically integrated atmospheric water flux divergence ($3^{rd}$ panel), and relative changes in the mean precipitation ($4^{th}$ panel), calculated from the CRCM simulation for the winter season from December 2040 to February 2070. Units are in mm/day.}\label{Fig10}
\end{figure}

% Figure 11
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig11}
  \caption{Relative changes in the climatological intraseasonal standard deviation of precipitation ($1^{st}$ panel), evapotranspiration ($2^{nd}$ panel), vertically integrated atmospheric water flux divergence ($3^{rd}$ panel) and vertically integrated water vapour tendency ($4^{th}$ panel), calculated from the CRCM simulation for the winter season from December 2040 to February 2070.}\label{Fig11}
\end{figure}

% Figure 12 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig12}
  \caption{Changes in the climatological intraseasonal variance of the total (top row), large-scale component (middle row) and small-scale component plus covariance (bottom row) of precipitation ($1^{st}$ column), evapotranspiration ($2^{nd}$ column), vertically integrated atmospheric water flux divergence ($3^{rd}$ column) and vertically integrated water vapour tendency ($4^{th}$ column), calculated from the CRCM simulation for the winter season from December 2040 to February 2070. Units are in mm$^2$/day$^2$.}\label{Fig12}
\end{figure}

% Figure 13 
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.25\textwidth]{Fig13}
  \caption{Changes in the climatological intraseasonal variance of the total vertically integrated atmospheric water flux divergence (top row), its CGCM3-resolved contribution (middle row), and its CGCM3-unresolved contribution plus covariance (bottom row), calculated on pressure levels from the CRCM simulation for the winter season from December 2040 to February 2070. Units are in mm$^2$/day$^2$.}\label{Fig13}
\end{figure}

% Figure 14
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.75\textwidth]{Fig14}
  \caption{Relative changes in the climatological intraseasonal standard deviation of the nine interaction terms entering the vertically integrated atmospheric water flux divergence, calculated on pressure levels from the CRCM simulation for the winter season from December 2040 to February 2070.}\label{Fig14}
\end{figure}

% Figure 15
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig15}
  \caption{Same as \ref{Fig10} but for the summer season from June 2041 to August 2070.}\label{Fig15}
\end{figure}

% Figure 16
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig16}
  \caption{Same as \ref{Fig11} but for the summer season from June 2041 to August 2070.}\label{Fig16}
\end{figure}

% Figure 17
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=\textwidth]{Fig17}
  \caption{Same as \ref{Fig12} but for the summer season from June 2041 to August 2070.}\label{Fig17}
\end{figure}

% Figure 18
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.25\textwidth]{Fig18}
  \caption{Same as \ref{Fig13} but for the summer season from June 2041 to August 2070.}\label{Fig18}
\end{figure}

% Figure 19
\clearpage
\begin{figure}[c]
  \centering
  \noindent\includegraphics[width=0.75\textwidth]{Fig19}
  \caption{Same as \ref{Fig14} but for the summer season from June 2041 to August 2070.}\label{Fig19}
\end{figure}



