[cig-commits] r20504 - in seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL: . figures

[dkomati1 at geodynamics.org]

Author: dkomati1
Date: 2012-07-07 17:19:03 -0700 (Sat, 07 Jul 2012)
New Revision: 20504

Modified:
   seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/figures/specfem_3d_globe-cover.ai
   seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/figures/specfem_3d_globe-cover.pdf
   seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/manual_SPECFEM3D_GLOBE.pdf
   seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/manual_SPECFEM3D_GLOBE.tex
   seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/specfem_3d_globe-cover_small.jpg
Log:
updated the manual


Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/figures/specfem_3d_globe-cover.ai
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Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/figures/specfem_3d_globe-cover.pdf
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Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/manual_SPECFEM3D_GLOBE.pdf
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Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/manual_SPECFEM3D_GLOBE.tex
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--- seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/manual_SPECFEM3D_GLOBE.tex	2012-07-07 23:59:26 UTC (rev 20503)
+++ seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/manual_SPECFEM3D_GLOBE.tex	2012-07-08 00:19:03 UTC (rev 20504)
@@ -105,10 +105,7 @@
 The SPECFEM3D\_GLOBE package was first developed by Dimitri Komatitsch and Jeroen Tromp at Harvard University and Caltech, USA, starting in 1998, based on earlier work by Dimitri Komatitsch and Jean-Pierre Vilotte at Institut de Physique du Globe (IPGP) in Paris, France from 1995 to 1997.\\
 
 Since then it has been developed and maintained by a development team: in alphabetical order,
-Piero Basini,
-C\'eline Blitz,
 Ebru Bozda\u{g},
-Emanuele Casarotti,
 Joseph Charles,
 Min Chen,
 Vala Hj\"orleifsd\'ottir,
@@ -120,13 +117,14 @@
 Qinya Liu,
 Yang Luo,
 Alessia Maggi,
-Federica Magnoni,
 Roland Martin,
 Dennis McRitchie,
 Matthias Meschede,
+% Peter Messmer,  % uncomment for future version 6.0 with GPU support, and put on the cover and Web icon as well
 David Mich\'ea,
 Tarje Nissen-Meyer,
 Daniel Peter,
+% Max Rietmann,  % uncomment for future version 6.0 with GPU support, and put on the cover and Web icon as well
 Brian Savage,
 Bernhard Schuberth,
 Anne Sieminski,
@@ -155,7 +153,7 @@
 
 It has very good accuracy and convergence properties \citep{MaPa89,SePr94,DeFiMu02,Coh02,DeSe07,SeOl08}.
 The spectral element approach admits spectral rates of convergence and allows exploiting $hp$-convergence schemes.
-It is also very well suited to parallel implementation on very large supercomputers \citep{KoTr02a,KoTsChTr03,TsKoChTr03,KoLaMi08a,CaKoLaTiMiLeSnTr08,KoViCh10} as well as on clusters of GPU accelerating graphics cards \citep{KoMiEr09,KoErGoMi10,Kom11}. Tensor products inside each element can be optimized to reach very high efficiency \citep{DeFiMu02}, and mesh point and element numbering can be optimized to reduce processor cache misses and improve cache reuse \citep{KoLaMi08a}. The SEM can also handle triangular (in 2D) or tetrahedral (in 3D) elements \citep{WinBoyd96,TaWi00,KoMaTrTaWi01,Coh02,MeViSa06} as well as mixed meshes, although with increased cost and reduced accuracy in these elements, as in the discontinuous Galerkin method.\\
+It is also very well suited to parallel implementation on very large supercomputers \citep{KoTsChTr03,TsKoChTr03,KoLaMi08a,CaKoLaTiMiLeSnTr08,KoViCh10} as well as on clusters of GPU accelerating graphics cards \citep{KoMiEr09,KoErGoMi10,Kom11}. Tensor products inside each element can be optimized to reach very high efficiency \citep{DeFiMu02}, and mesh point and element numbering can be optimized to reduce processor cache misses and improve cache reuse \citep{KoLaMi08a}. The SEM can also handle triangular (in 2D) or tetrahedral (in 3D) elements \citep{WinBoyd96,TaWi00,KoMaTrTaWi01,Coh02,MeViSa06} as well as mixed meshes, although with increased cost and reduced accuracy in these elements, as in the discontinuous Galerkin method.\\
 
 Note that in many geological models in the context of seismic wave propagation studies
 (except for instance for fault dynamic rupture studies, in which very high frequencies or supershear rupture need to be modeled near the fault, see e.g. \cite{BeGlCrViPi07,BeGlCrVi09,PuAmKa09,TaCrEtViBeSa10})

Modified: seismo/3D/SPECFEM3D_GLOBE/trunk/doc/USER_MANUAL/specfem_3d_globe-cover_small.jpg
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