CVM-H 15.1 Maps - Revision history

Maechlin at 16:42, 1 July 2018

2018-07-01T16:42:11Z

2018-07-01T16:41:03Z

2018-07-01T16:40:18Z

2018-07-01T16:35:06Z

CVM-H GTL Plot

2018-07-01T16:34:36Z

Related Entries

2018-07-01T00:52:48Z

2018-06-30T22:55:00Z

2018-06-30T22:51:12Z

2018-06-30T22:50:00Z

CVM-H 15.1 Near Surface Properties with and without optional Ely-Jordan GTL

2018-06-30T22:49:39Z

@@ Line 1: / Line 1: @@
 == Ely Jordan GTL Documentation ==
 *[http://hypocenter.usc.edu/research/UCVM/Ely-Vs30GTL.pdf Ely GTL Method Writeup]
-*[http://hypocenter.usc.edu/research/UCVM/Seismic Velocity Model.webarchive Ely GTL Web archive]
+*[http://hypocenter.usc.edu/research/UCVM/SeismicVelocityModel.webarchive Ely GTL Web archive]
 == CVM-H Near Surface Plots ==

@@ Line 1: / Line 1: @@
 == Ely Jordan GTL Documentation ==
-*[http://hypocenter.usc.edu/research/UCVM/ElyVs30GTL.pdf Ely GTL Method Writeup]
+*[http://hypocenter.usc.edu/research/UCVM/Ely-Vs30GTL.pdf Ely GTL Method Writeup]
 *[http://hypocenter.usc.edu/research/UCVM/Seismic Velocity Model.webarchive Ely GTL Web archive]

← Older revision		Revision as of 16:40, 1 July 2018
Line 1:		Line 1:
		+	== Ely Jordan GTL Documentation ==
		+	*[http://hypocenter.usc.edu/research/UCVM/ElyVs30GTL.pdf Ely GTL Method Writeup]
		+	*[http://hypocenter.usc.edu/research/UCVM/Seismic Velocity Model.webarchive Ely GTL Web archive]
		+
		+	== CVM-H Near Surface Plots ==
	The plots below show the characteristics of the CVM-H v15.1 velocity model for the Los Angeles region. The four columns show model properties including Vp, Vs, Density, and Vp/Vs Ratio.		The plots below show the characteristics of the CVM-H v15.1 velocity model for the Los Angeles region. The four columns show model properties including Vp, Vs, Density, and Vp/Vs Ratio.
	There are multiple rows of data at depths 0m, 100m, 300m, and 500m. The expectation is that the GTL will affect the top 350m but not deeper. This plots the surface 0m, then 100m, 300m, and 500m.		There are multiple rows of data at depths 0m, 100m, 300m, and 500m. The expectation is that the GTL will affect the top 350m but not deeper. This plots the surface 0m, then 100m, 300m, and 500m.

@@ Line 90: / Line 90: @@
 == CVM-H GTL Plot ==
-*[[File:Cvm-h vs30gtl.png|thumb|300px]]
+*[[File:Cvm-h vs30gtl.png|thumb|300px|left]]
 == Related Entries ==
 *[[UCVM]]

@@ Line 88: / Line 88: @@
 *Plots, points (json format), and data (bin format) are posted online at: [http://hypocenter.usc.edu/research/UCVM/cvmh_no_ely_gtl/ Default CVM-H Map Plots and Data]
 *Plots, points (json format), and data (bin format) are posted online at: [http://hypocenter.usc.edu/research/UCVM/cvmh_ely_gtl/ CVM-H with ElyGTL Map Plots and Data]
 == Related Entries ==
 *[[UCVM]]

@@ Line 1: / Line 1: @@
 The plots below show the characteristics of the CVM-H v15.1 velocity model for the Los Angeles region. The four columns show model properties including Vp, Vs, Density, and Vp/Vs Ratio.
-There are multiple rows of data at depths 0m, 100m, 300m, and 500m. The expectation is that the GTL will affect the top 350m but not deeper. This plots the surface, then 100m, 300m, and 500m.
+There are multiple rows of data at depths 0m, 100m, 300m, and 500m. The expectation is that the GTL will affect the top 350m but not deeper. This plots the surface 0m, then 100m, 300m, and 500m.
 There are two rows for each, one with the original CVM-H properties, and one with the Ely-Jordan GTL added.  One consideration is that the CVM-H model is defined as query by elevation. UCVM accepts the query by depth, and converts it into a query by elevation internally. This could be a source of artifacts of properties at 0 depth.

@@ Line 24: / Line 24: @@
 | [[Image:cvmh_gtl_density_0_map.png |thumb|300px]]
 | [[Image:cvmh_gtl_poisson_0_map.png |thumb|300px]]
 |-
 | 100m - CVM-H
@@ Line 87: / Line 86: @@
 |}
-*Plots, points (json format), and data (bin format) are posted online at: [http://hypocenter.usc.edu/research/UCVM/cvmh_no_ely_gtl/ CVM-H Map Plots and Data]
+*Plots, points (json format), and data (bin format) are posted online at: [http://hypocenter.usc.edu/research/UCVM/cvmh_no_ely_gtl/ Default CVM-H Map Plots and Data]
-*Plots, points (json format), and data (bin format) are posted online at: [http://hypocenter.usc.edu/research/UCVM/cvmh_ely_gtl/ CVM-H Map Plots and Data]
+*Plots, points (json format), and data (bin format) are posted online at: [http://hypocenter.usc.edu/research/UCVM/cvmh_ely_gtl/ CVM-H with ElyGTL Map Plots and Data]
 == Related Entries ==
 *[[UCVM]]

← Older revision		Revision as of 22:49, 30 June 2018
Line 1:		Line 1:
		+	The plots below show the characteristics of the CVM-H v15.1 velocity model for the Los Angeles region. The four columns show model properties including Vp, Vs, Density, and Vp/Vs Ratio.
		+	There are multiple rows of data at depths 0m, 100m, 300m, and 500m. The expectation is that the GTL will affect the top 350m but not deeper. This plots the surface, then 100m, 300m, and 500m.
		+	There are two rows for each, one with the original CVM-H properties, and one with the Ely-Jordan GTL added. One consideration is that the CVM-H model is defined as query by elevation. UCVM accepts the query by depth, and converts it into a query by elevation internally.
		+
	== CVM-H 15.1 Near Surface Properties with and without optional Ely-Jordan GTL ==		== CVM-H 15.1 Near Surface Properties with and without optional Ely-Jordan GTL ==
	{\| class ="wikitable"		{\| class ="wikitable"