Changeset 3166

Timestamp:

Jun 15, 2006, 5:46:47 PM (18 years ago)

Author:

sexton

Message:

fixing stuffups

Location:

production/onslow_2006/report

Files:

• modelling_methodology.tex (modified) (1 diff)
• references.tex (modified) (1 diff)

production/onslow_2006/report/modelling_methodology.tex

@@ -6 +6 @@
 resolution of 2 arc minutes (check this with David). Near a coastline the maximal wave height at a fixed contour line (e.g.\ 50m) is then reported as the 
 hazard to communities ashore. 
-Models such as Method of Splitting Tsunamies (MOST) \cite{VT:MOST} and ``URS model'' \cite{xxx} follow this paradigm.
+Models such as Method of Splitting Tsunamies (MOST) \cite{VT:MOST} and ``URS model'' \cite{person:urs} follow this paradigm.
 
 To capture the \emph{impact} of a hydrological disaster such as tsunamies on a community one must model the the details of how waves are reflected and otherwise shaped by the local bathymetries as well as the dynamics of the runup process onto the topography in question.

production/onslow_2006/report/references.tex

@@ -4 +4 @@
 Small threat, but warning sounded for tsunami research. AusGeo News 75, 4-7.
 
-\bibitem{VT:most} Titov, V.V., and F.I. Gonzalez (1997)
+\bibitem{VT:MOST} Titov, V.V., and F.I. Gonzalez (1997)
 mplementation and testing of the Method of Splitting 
 Tsunami (MOST) model, NOAA Technical Memorandum ERL PMEL-112.