[cig-commits] r11869 - seismo/3D/automeasure/latex

[carltape at geodynamics.org]

Author: carltape
Date: 2008-04-29 13:51:00 -0700 (Tue, 29 Apr 2008)
New Revision: 11869

Modified:
   seismo/3D/automeasure/latex/AM-allcitations.bib
   seismo/3D/automeasure/latex/appendix.tex
   seismo/3D/automeasure/latex/flexwin_paper.pdf
Log:
Added user_functions.f90 parameters for socal into the appendix.


Modified: seismo/3D/automeasure/latex/AM-allcitations.bib
===================================================================
--- seismo/3D/automeasure/latex/AM-allcitations.bib	2008-04-29 19:34:22 UTC (rev 11868)
+++ seismo/3D/automeasure/latex/AM-allcitations.bib	2008-04-29 20:51:00 UTC (rev 11869)
@@ -6281,6 +6281,16 @@
 	Volume = 84,
 	Year = 1979}
 
+ at article{Wald95,
+     AUTHOR = {Wald, L. A. and Hutton, L. K. and Given, D. D.},
+     JOURNAL = srl,
+     PAGES = {9--19},
+     TITLE = {{The Southern California Network Bulletin: 1990--1993 summary}},
+     VOLUME = 66,
+     NUMBER = 1,
+     YEAR = 1995}
+
+
 @article{WalkerJB2003,
 	Author = {Walker, R. and   Jackson, J. and   Baker, C.},
 	Journal = gji,

Modified: seismo/3D/automeasure/latex/appendix.tex
===================================================================
--- seismo/3D/automeasure/latex/appendix.tex	2008-04-29 19:34:22 UTC (rev 11868)
+++ seismo/3D/automeasure/latex/appendix.tex	2008-04-29 20:51:00 UTC (rev 11869)
@@ -26,7 +26,7 @@
     0.95 & \text{$t > t_R$} 
   \end{cases}
 \\
-\tau_0(t) & = 
+\Delta\tau_0(t) & = 
   \begin{cases}
     \begin{cases}
       \tau_0 & \text{$t \leq t_R$} \\
@@ -46,16 +46,52 @@
 
 %--------------------------
 
+\pagebreak
 \subsection{Japan scenario\label{ap:user_japan}}
 
 MIN: fill this in please.
 
 %--------------------------
 
+\pagebreak
 \subsection{Southern California scenario\label{ap:user_socal}}
 
-Below $t_P$, $t_S$, $t_{R0}$ denote the start of the time windows for the crustal P wave, the crustal S wave, and, and the crustal surface wave, respectively, computed using a 1D layered model. The end time of the surface-wave window is given by $t_{R1}$.
+Below $t_P$ and $t_S$ denote the start of the time windows for the crustal P wave and the crustal S wave, computed from a 1D layered model \citep{Wald95}.  The start and finish times for the surface-wave time window, $t_{R0}$ and $t_{R1}$, as well as the criteria for the time-shifts $\Delta\tau_0(t)$, are computed from the formulas in \cite{KomatitschEtal2004}. The source-receiver distance (in km) is denoted by $\Delta$.
 
-CARL: fill this in please.
+For the \trange{6}{40} data, we use
+%
+\begin{align}
+w_E(t) & =
+  \begin{cases}
+    10 w_E & \text{$t < t_P$} \\
+    w_E & \text{$t_P \le t \leq t_{R1}$} \\
+    2 w_E & \text{$t > t_{R1}$}
+  \end{cases}
+\\
+r_0(t) & = r_0
+\\
+CC_0(t) & = CC_0
+\\
+\Delta\tau_0(t) & = 
+  \begin{cases}
+    3.0 + \Delta/80.0 & \text{$t \le t_{R0}$} \\
+    3.0 + \Delta/50.0 & \text{$t > t_{R0}$}
+  \end{cases}
+\\
+\Delta \ln A_0(t) & = \Delta \ln A_0 
+\end{align}
 
+For the \trange{2}{40} data, we avoid selecting surface-wave arrivals, and therefore we make the modifications
+%
+\begin{align}
+w_E(t) & =
+  \begin{cases}
+    10 w_E & \text{$t < t_P$} \\
+    w_E & \text{$t_P \le t \leq t_S$} \\
+    10 w_E & \text{$t > t_S$}
+  \end{cases}
+\\
+\Delta\tau_0(t) & = \Delta\tau_0
+\end{align}
+
 %--------------------------

Modified: seismo/3D/automeasure/latex/flexwin_paper.pdf
===================================================================
(Binary files differ)