[GRASS-SVN] r59761 - grass-promo/grassposter/2014_EGU_WD_Landscape

[svn_grass at osgeo.org]

Author: ychemin
Date: 2014-04-17 03:46:23 -0700 (Thu, 17 Apr 2014)
New Revision: 59761

Modified:
   grass-promo/grassposter/2014_EGU_WD_Landscape/poster.tex
Log:
update credits

Modified: grass-promo/grassposter/2014_EGU_WD_Landscape/poster.tex
===================================================================
--- grass-promo/grassposter/2014_EGU_WD_Landscape/poster.tex	2014-04-17 06:39:58 UTC (rev 59760)
+++ grass-promo/grassposter/2014_EGU_WD_Landscape/poster.tex	2014-04-17 10:46:23 UTC (rev 59761)
@@ -163,29 +163,18 @@
 %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
 \blocknode{Acknowledgements}{
 \smallskip
-The authors would like to acknowledge the CGIAR Research Program on Water, Land and Ecosystems (WLE ; \url{wle.cgiar.org}) Innovation Fund.\newline
+\begin{tabular}{p{0.70\textwidth} c}
+	The authors would like to acknowledge the CGIAR Research Program on Water, Land and Ecosystems (WLE ; \url{wle.cgiar.org}) Innovation Fund.
+	&
+	\hspace{3mm}
+	\raisebox{-0.5\totalheight}{\includegraphics[width=0.27\textwidth]{./images/WLE}}
+\end{tabular}
 }
 
 
 \startthirdcolumn
 
 %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
-\blocknode{Temporal patterns of recession cropping \& natural vegetation}{
-
-\begin{center}
-	\begin{tabular}{cc}
-	\raisebox{-0.5\totalheight}{\includegraphics[width=0.45\textwidth]{./images/MSUBAS_TS}}
-	&
-	\begin{tabular}{p{0.5\textwidth}}
- 	\includegraphics[width=0.45\textwidth]{./svg_images/EVI_distance_from_tonle_sap}\\
-	The results for TSC show that the range between $EVI_{min}$ and $EVI_{max}$ in floodplains surrounding the Tonle Sap Lake decreases spatially with distance from dry season margins of the lake. This pattern is indicative of flood recession cropping systems and seasonally flooded natural vegetation around the lake, which expands dramatically in size during the wet season each year, inundating large areas of floodplain, which drain towards the dry season.  We used the blue band of MOD13 to provide an additional indicator of flooding, handling the assumption of seasonal flood occurrence if ‘Blue’ approaches or exceeds ‘EVI’. The results in TSC do not discern any long-term trends in land cover and land use.\newline
-	\end{tabular}
- 	\end{tabular}\newline
-\end{center}
-
-}
-
-%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
 \blocknode{From recession cropping (UL) to natural vegetation (LR)}{
 \begin{center}
 	\begin{tabular}{cc}
@@ -204,6 +193,22 @@
 }
 
 %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
+\blocknode{Temporal patterns of recession cropping \& natural vegetation}{
+
+\begin{center}
+	\begin{tabular}{cc}
+	\raisebox{-0.5\totalheight}{\includegraphics[width=0.45\textwidth]{./images/MSUBAS_TS}}
+	&
+	\begin{tabular}{p{0.5\textwidth}}
+ 	\includegraphics[width=0.45\textwidth]{./svg_images/EVI_distance_from_tonle_sap}\\
+	The results for TSC show that the range between $EVI_{min}$ and $EVI_{max}$ in floodplains surrounding the Tonle Sap Lake decreases spatially with distance from dry season margins of the lake. This pattern is indicative of flood recession cropping systems and seasonally flooded natural vegetation around the lake, which expands dramatically in size during the wet season each year, inundating large areas of floodplain, which drain towards the dry season.  We used the blue band of MOD13 to provide an additional indicator of flooding, handling the assumption of seasonal flood occurrence if ‘Blue’ approaches or exceeds ‘EVI’. The results in TSC do not discern any long-term trends in land cover and land use.\newline
+	\end{tabular}
+ 	\end{tabular}\newline
+\end{center}
+
+}
+
+%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%
 \blocknode{GRASS GIS script for MODIS PCA \& segmentation of PCA}{
 \smallskip
 {\footnotesize \fontfamily{pcr}\selectfont