[Dart-dev] [3320] group/posters/trunk/2008_AMS/2008_AMS_hui.tex: final syntax tweaks by Tim

[thoar at subversion.ucar.edu]

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Modified: group/posters/trunk/2008_AMS/2008_AMS_hui.tex
===================================================================
--- group/posters/trunk/2008_AMS/2008_AMS_hui.tex	2008-04-22 23:27:51 UTC (rev 3319)
+++ group/posters/trunk/2008_AMS/2008_AMS_hui.tex	2008-04-23 14:47:34 UTC (rev 3320)
@@ -16,7 +16,7 @@
        Innovative GPSRO Satellite Observations}
 
 % Note: only give author names, not institute
-\author{H.~Liu, J.~Anderson, Y.-H.~Kuo, Y. ~Chen, and C.~Snyder}
+\author{H.~Liu, J.~Anderson, Y.-H.~Kuo, Y.~Chen, and C.~Snyder}
 
 % insert institute name
 \institute{National Center for Atmospheric Research\\
@@ -55,7 +55,7 @@
 \begin{center}
 \includegraphics[height=0.4\columnwidth,angle=0]{best_shan_track.pdf}
 \end{center}
-\caption{Observed best track and intensity of Typhoon Shanshan (2006).}
+\caption{Observed Best Track and intensity of Typhoon Shanshan (2006).}
 \label{fig:best_track}
 \end{figure}
 
@@ -94,9 +94,10 @@
 
 \begin{figwindow}[0,r, %
 {\fbox{\includegraphics[height=0.47\columnwidth,angle=0]{gloc13aug.png}}},%
-{Locations of RO profiles over the Western Pacific domain, September 13, 2006.}]
-During 13 September 2006, there were 24 GPS RO refractivity profiles available over the 
-Western Pacific domain. These observations provided large-scale water vapor information.
+{Locations of RO profiles over the Western Pacific domain, 13 September 2006.}]
+There were 24 GPS RO refractivity profiles available over the Western Pacific 
+domain for 13 September 2006.
+These observations provided large-scale water vapor information.
 \end{figwindow}
 
 \vspace{2.0in}
@@ -109,7 +110,7 @@
 \subsection{WRF/DART Ensemble Assimilation System}
 
 NCAR's Weather and Research Forecast (WRF) model is a state-of-the-art mesoscale
-atmospheric model.  The NCAR WRF/DART (Data Assimilation Research Testbed)
+atmospheric model.  The NCAR DART (Data Assimilation Research Testbed)
 ensemble data assimilation system 
 is used to assimilate the observations into WRF, which is then run in forecast mode.
 This ensemble-based system is particularly good for mesoscale analysis because 
@@ -153,9 +154,9 @@
 \subsection{Impact on track forecast}
 
 The left panel of Figure~\protect\ref{fig:ens_track} depicts the performance of the
-`NOGPS' experiment. The best track is not in the center of the tracks of the ensemble
+`NOGPS' experiment. The Best Track is not in the center of the tracks from the ensemble
 members. The panel on the right is the result of the `GPS' experiment. 
-The ensemble tracks are more symmetrically distributed around the best track and result 
+The ensemble tracks are more symmetrically distributed around the Best Track and result 
 in an ensemble mean that is much more representative of the Best Track. 
 With the GPS RO observations, the ensemble performs better, especially at the later 
 stage of the forecasts.