[cig-commits] r11379 - in seismo/3D/automeasure/latex: . figures/socal

carltape at geodynamics.org carltape at geodynamics.org
Fri Mar 7 18:12:46 PST 2008 

Author: carltape
Date: 2008-03-07 18:12:46 -0800 (Fri, 07 Mar 2008)
New Revision: 11379

Added:
   seismo/3D/automeasure/latex/figures/socal/9818433_CLC_window.eps
   seismo/3D/automeasure/latex/figures/socal/9818433_FMP_window.eps
   seismo/3D/automeasure/latex/figures/socal/9983429_T02_rs.eps
   seismo/3D/automeasure/latex/figures/socal/9983429_T06_rs.eps
Modified:
   seismo/3D/automeasure/latex/README
   seismo/3D/automeasure/latex/figures_paper.tex
   seismo/3D/automeasure/latex/flexwin_paper.pdf
   seismo/3D/automeasure/latex/results.tex
Log:
Updates to paper.


Modified: seismo/3D/automeasure/latex/README
===================================================================
--- seismo/3D/automeasure/latex/README	2008-03-07 23:20:06 UTC (rev 11378)
+++ seismo/3D/automeasure/latex/README	2008-03-08 02:12:46 UTC (rev 11379)
@@ -1,3 +1,23 @@
-Carl Tape, 05-Feb-2008
+Carl Tape, 07-March-2008
 
+This file: /automeasure/latex/figures/socal/README
+
 To compile from Caltech, use pdflatex.
+
+Convert eps figures to pdf using epstopdf.
+
+------------------------------
+07-March-2008
+
+I have finally added my figures and text, but I have not made substantial changes to other sections.  The bulleted numbered lists follow the format of GJI, although I am not a big fan of them.  I bulleted a few sets of notes, which will eventually turn into text.
+
+Min, I think the next step is for you to add your figures and text to the paper, and also the parts of the tables left for you.  If you choose to use Adobe Illustrator, then you can see my AI EPS files here, if you want to use them as templates:
+
+/net/denali/scratch1/carltape/svn/cig/seismo/3D/automeasure_work/latex/figures/socal/
+
+These were made on a Mac using CS3.  The outlines guaranteed that related figures were exactly the same size, but we can get rid of the lines in the end if we want to.
+
+Alessia, it sounds like Min can get her edits committed within one week, hopefully sooner.  Then perhaps you can take another run-though at the text, then we can quickly, and then we can send it to Jeroen.
+
+I think it is going to be a great paper.  I think if we all focus our efforts now, we can submit it within a couple weeks.
+------------------------------

Added: seismo/3D/automeasure/latex/figures/socal/9818433_CLC_window.eps
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Modified: seismo/3D/automeasure/latex/figures_paper.tex
===================================================================
--- seismo/3D/automeasure/latex/figures_paper.tex	2008-03-07 23:20:06 UTC (rev 11378)
+++ seismo/3D/automeasure/latex/figures_paper.tex	2008-03-08 02:12:46 UTC (rev 11379)
@@ -278,6 +278,7 @@
 %\center
 \includegraphics[width=7in]{figures/socal/9983429_T02_rs.pdf}
 \caption{\label{fg:socal_rs_T02} 
+(THIS FIGURE COULD IN THEORY BE CUT OUT, IF SPACE IS SHORT.)
 Summary plots of windowing results for event 9983429 in Table~\ref{tb:events}, for the period range 2~s to 40~s.
 Same as Figure~\ref{fg:socal_rs_T06}, only the windowing code has been run using a different set of parameters (Table~\ref{tb:example_params}), so that primarily only the body-wave arrivals are selected.
 }

Modified: seismo/3D/automeasure/latex/flexwin_paper.pdf
===================================================================
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Modified: seismo/3D/automeasure/latex/results.tex
===================================================================
--- seismo/3D/automeasure/latex/results.tex	2008-03-07 23:20:06 UTC (rev 11378)
+++ seismo/3D/automeasure/latex/results.tex	2008-03-08 02:12:46 UTC (rev 11379)
@@ -35,13 +35,13 @@
 
 \pagebreak
 
-{\bf Can we each follow this outline for each section?}
+{\bf We follow this outline for the text in each section}
 %
 \begin{enumerate}
+\item Describe structure and forward model.
 \item Describe sources.
-\item Describe structure and forward model.
 \item Described figures.
-\item Summarize the dataset.
+\item Optional: Summarize the dataset.
 \end{enumerate}
 
 %----------------------------------------
@@ -183,8 +183,7 @@
 \subsection{Southern California scale}
 \label{sec:socal}
 
-We next apply the windowing code to a set of 150 events within southern California.  The events, with $M_w$ magnitudes between 3.5 and 5.5, were recorded between 1999 and 2007 and constitute a subset of the focal mechanisms presented by \citet{Clinton06}.  The locations and origin times are primarily from \citet{LSHsource}, supplemented by the catalog of \citet{Thurber06} for events near Parkfield and the catalog of \citet{McLaren08} for events near San Simeon.  Each of these regions had $M_w > 6$ earthquakes within our time period of interest: 2004.09.28~$M_w$~6.0 near Parkfield and 2003.12.22~$M_w$~6.5 near San Simeon. Aftershocks of both events are included in the dataset.
-
+We next apply the windowing code to a set of 150 events within southern California.
 We compute synthetic seismograms using the spectral-element method for a regional 3D crustal and upper mantle model for southern California \citep{Koma04}.  This model contains three discontinuities:
 %
 \begin{enumerate}
@@ -195,8 +194,10 @@
 %
 The basement surface is essential for simulating the resonance of seismic waves within sedimentary basins, such as the Ventura basin, the L.A. basin, and the Salton trough \citep{Koma04,Lovely06}. The smooth 3D background velocity model used in \citet{Koma04} was \citet{Hauksson00}; we use an updated version provided by \citet{LSHtomo}. The physical domain of the model is approximately 600~km by 500~km at the surface, and extends to a depth of 60~km. Our simulations of seismic waves are numerically accurate down to a period of 1.5~s.
 
-We test the windowing code for 150 events using two period ranges: 6--40~s and 2--40~s.  The parameters we use for the windowing code are listed in Table~\ref{tb:example_params}.  Figures~\ref{fg:socal_rs_T06}--\ref{fg:socal_FMP} show examples of the output from the windowing code for the two events listed in Table~\ref{tb:events}: 2002.09.03~$M_w$~4.3 and 2004.02.14~$M_w$~4.6.
+The 150 events, with $M_w$ magnitudes between 3.5 and 5.5, were recorded between 1999 and 2007 and constitute a subset of the focal mechanisms presented by \citet{Clinton06}.  The locations and origin times are primarily from \citet{LSHsource}, supplemented by the catalog of \citet{Thurber06} for events near Parkfield and the catalog of \citet{McLaren08} for events near San Simeon.  Each of these regions had $M_w > 6$ earthquakes within our time period of interest: 2004.09.28~$M_w$~6.0 near Parkfield and 2003.12.22~$M_w$~6.5 near San Simeon. Aftershocks of both events are included in the dataset.
 
+We test the windowing code using two period ranges: 6--40~s and 2--40~s.  The parameters we use for the windowing code are listed in Table~\ref{tb:example_params}.  Figures~\ref{fg:socal_rs_T06}--\ref{fg:socal_FMP} show examples of the output from the windowing code for the two events listed in Table~\ref{tb:events}: 2002.09.03~$M_w$~4.3 and 2004.02.14~$M_w$~4.6.
+
 Figures~\ref{fg:socal_rs_T06} and \ref{fg:socal_rs_T02} show summary plots of the window picks for one event for the two different period ranges, each which has a different set of parameters (Table~\ref{tb:example_params}). The window record section in Figure~\ref{fg:socal_rs_T06} illuminates the primary phases that are picked by the algorithm. On the vertical and radial components, the first branch corresponds to body-wave arrivals, and the second branch corresponds to the Rayleigh-wave arrival. Windows on the transverse component capture the Love wave arrival.
 
 Figure~\ref{fg:socal_rs_T02} shows the window picks for the same event as in Figure~\ref{fg:socal_rs_T06}, only for the period range 2--40~s instead of 6--40~s. Because the majority of the synthetic seismograms do not agree well with the observed seismograms, we raise the water level associated with the STA:LTA curve (dashed line in Figure~\ref{fg:socal_CLC}e) so that primarily only body-wave arrivals are picked. The result is that prominent Rayleigh-wave and Love-wave branches in Figure~\ref{fg:socal_rs_T06} are not observed in Figure~\ref{fg:socal_rs_T02}.

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