Difference between revisions of "La Habra Simulations on Titan"

From SCECpedia
Jump to navigationJump to search
 
(24 intermediate revisions by 2 users not shown)
Line 38: Line 38:
 
|-
 
|-
 
| Station List
 
| Station List
−
| [[File:lahabra_titan_stations.txt]]
+
| [http://earth.usc.edu/~patrices/hercules/lahabra/LH_stations.txt LH_stations.txt]
−
| ?
+
| Merged from En-Jui's 0.2Hz station list and Ricardo's CH master list
 
|-
 
|-
 
| Software Version
 
| Software Version
−
| Hercules-GPU i3
+
| Hercules-GPU commit c95f1ab017e5f93613a0e3e2c6b5a849eb4117ad
−
| GPU codes, no freqency dependent Q
+
| GPU codes, no frequency dependent Q
 
|}
 
|}
  
Line 69: Line 69:
 
|-
 
|-
 
| Velocity Model Versions
 
| Velocity Model Versions
−
| CVM-S4, CVM-S4 v26, CVM-S5
+
| CVM-S4, CVM-S4 v26
−
|
+
| CVM-S5?
 
|-  
 
|-  
 
|Miniumum Vs
 
|Miniumum Vs
Line 86: Line 86:
  
  
−
== Source Parameters ==
+
== Sources ==
 +
 
 +
The simulation will be repeated for two point sources and one extended source.
 +
 
 +
=== Point Source Parameters ===
  
 
{| class="wikitable" border="1"
 
{| class="wikitable" border="1"
Line 106: Line 110:
 
| Source: En-Jui
 
| Source: En-Jui
 
|-
 
|-
−
| Strike/Dip/Rake
+
| Strike/Dip/Rake 1
 
| 134/55/155
 
| 134/55/155
−
| Source: En-Jui
+
| Source: En-Jui, initial
 +
|-
 +
| Strike/Dip/Rake 2
 +
| 239/70/38
 +
| Source: En-Jui, based on review of aftershock sequence
 +
|-
 +
| Rise Time
 +
| 0.75 s
 +
|
 
|-
 
|-
−
| Slip Function
+
| Origin X/Y
−
| ?
+
| [http://earth.usc.edu/~patrices/hercules/lahabra/EQ_lahabra_xy.list EQ_lahabra_xy.list]
−
| ?
+
|  
 
|}
 
|}
  
  
−
== SRC Format La Habra Source ==
+
=== SRC Format La Habra Source ===
−
*MAGNITUDE = 5.39
+
*MAGNITUDE = 5.12
−
*FAULT_LENGTH = 6.30
+
*FAULT_LENGTH = 5.0
−
*FAULT_WIDTH = 4.60
+
*FAULT_WIDTH = 2.25
−
*DEPTH_TO_TOP = 12.79
+
*DEPTH_TO_TOP = 4.7125
−
*STRIKE = 296
+
*STRIKE = 239
−
*RAKE = 146
+
*RAKE = 38
−
*DIP = 66
+
*DIP = 70
−
*LAT_TOP_CENTER = 33.939
+
*LAT_TOP_CENTER = 33.9119
−
*LON_TOP_CENTER = -117.771
+
*LON_TOP_CENTER = -117.940
 
*HYPO_ALONG_STK = 0.0
 
*HYPO_ALONG_STK = 0.0
−
*HYPO_DOWN_DIP = 2.30
+
*HYPO_DOWN_DIP = 1.125
 +
*DLEN = 0.1
 +
*DWID = 0.1
 +
 
 +
== Volume ==
 +
 
 +
The four corners are:
 +
*  -119.288842    34.120549
 +
*  -118.354016    35.061096
 +
*  -116.846030    34.025873
 +
*  -117.780976    33.096503
 +
 
 +
And the box has size
 +
*180,000 m x 135,000 m x 61,875 m
 +
 
 +
== Runs ==
 +
 
 +
 
 +
=== Hercules Runs ===
 +
 
 +
{| class="wikitable" border="1"
 +
|-
 +
! Run Number
 +
! Etree
 +
! Source
 +
! Notes
 +
|-
 +
| 1
 +
| ch-cvms400-100-4hz-200ms.e
 +
| point-ricardo-134-55-155
 +
|
 +
|-
 +
| 2
 +
| ch-cvms426-223-4hz-200ms.e
 +
| point-ricardo-134-55-155
 +
|
 +
|-
 +
| 3
 +
| ch-cvms400-100-4hz-200ms.e
 +
| point-ricardo-239-70-38
 +
|
 +
|-
 +
| 4
 +
| ch-cvms426-223-4hz-200ms.e
 +
| point-ricardo-239-70-38
 +
|
 +
|-
 +
| 5
 +
| ch-cvms400-100-4hz-200ms.e
 +
| extended-ricardo
 +
|
 +
|-
 +
| 6
 +
| ch-cvms426-223-4hz-200ms.e
 +
| extended-ricardo
 +
|
 +
|}
 +
 
 +
 
 +
=== BBP Run ===
 +
*[http://bbpvault.usc.edu/bbp/tests/la_habra/run1/la_habra_2014_06_19.src SRC for this event]
 +
 
 +
*[http://bbpvault.usc.edu/bbp/tests/la_habra/run1/la_habra_2014_06_19.png SRF Image]
 +
*[http://bbpvault.usc.edu/bbp/tests/la_habra/run1/la_habra_2014_06_19.srf SRF for this SRC]
 +
 
 +
 
 +
== La Habra Earthquake Observations ==
 +
*[http://strongmotioncenter.org/vdc/scripts/event.plx?evt=1295 Center for Strong Motion Engineering Data Center]
 +
 
 +
== La Habra References ==
 +
*[http://www.scsn.org/2014lahabra.html SCSN La Habra Event Summary]
 +
*[http://www.data.scec.org/MomentTensor/solutions/web_15481673/ci15481673_MT.html SCSN La Habra Moment Tensor Solution]
  
  
 
== References ==
 
== References ==
−
 
 
# Bielak, J., H. Karaoglu, and R. Taborda, 2011. Memory-efficient displacement-based internal friction for wave propagation simulation, Geophysics, 76(6):T131-T145.
 
# Bielak, J., H. Karaoglu, and R. Taborda, 2011. Memory-efficient displacement-based internal friction for wave propagation simulation, Geophysics, 76(6):T131-T145.
 
# Taborda, R., Lopez, J., Karaoglu, H., Urbanic, J., and Bielak, J. (2010). Speeding up finite element wave propagation for large-scale earthquake simulations. Technical Report CMU-PDL-10-109, Carnegie Mellon University, Parallel Data Lab.  
 
# Taborda, R., Lopez, J., Karaoglu, H., Urbanic, J., and Bielak, J. (2010). Speeding up finite element wave propagation for large-scale earthquake simulations. Technical Report CMU-PDL-10-109, Carnegie Mellon University, Parallel Data Lab.  
 
# Tu, T., Yu, H., Ramírez-Guzmán, L., Bielak, J., Ghattas, O., Ma, K.-L., & O’Hallaron, D.R., 2006. From mesh generation to scientific visualization: an end-to-end approach to parallel supercomputing, in Proceedings of the 2006 ACM/IEEE International Conference for High Performance Computing, Networking, Storage and Analysis, p. 15, IEEE Computer Society, Tampa, Florida.
 
# Tu, T., Yu, H., Ramírez-Guzmán, L., Bielak, J., Ghattas, O., Ma, K.-L., & O’Hallaron, D.R., 2006. From mesh generation to scientific visualization: an end-to-end approach to parallel supercomputing, in Proceedings of the 2006 ACM/IEEE International Conference for High Performance Computing, Networking, Storage and Analysis, p. 15, IEEE Computer Society, Tampa, Florida.

Latest revision as of 18:45, 16 July 2014

Overview

A series of simulations modelling the La Habra 5.1 event will be performed on ORNL Titan with in order to address these scientific and computational goals:

  • Demonstrate that Hercules-GPU software is in production status and evaluate its performance versus the CPU version
  • Evaluate goodness of fit for synthetic waveforms versus observed at 1.0 Hz, using Po Chen's updated CVM-S4 velocity model as the material properties source for the simulation.
  • [Optionally] Validate the simulation results generated by Hercules-GPU and AWP-GPU


Solver Parameters

Parameter Value Notes
Frequency 1.0 Hz
Simulation Length 100 s
Delta T 0.005
Plane Output Resolution 250m
I/O Print Rate every 10 steps
Station List LH_stations.txt Merged from En-Jui's 0.2Hz station list and Ricardo's CH master list
Software Version Hercules-GPU commit c95f1ab017e5f93613a0e3e2c6b5a849eb4117ad GPU codes, no frequency dependent Q


Simulation Box / Velocity Model

Parameter Value Notes
Dimensions (km) 180 x 135 x 61.875
Bounding Box (LL) -119.288842 34.120549, -118.354016 35.061096, -116.846030 34.025873, -117.780976 33.096503
UCVM Version 13.9.0 No heterogeneities
Velocity Model Versions CVM-S4, CVM-S4 v26 CVM-S5?
Miniumum Vs 200 m/s
Samples per wavelength 8
Hercules Etree ch-cvms400-100-4hz-200ms.e, ch-cvms426-223-4hz-200ms.e CVM-S5 etree?


Sources

The simulation will be repeated for two point sources and one extended source.

Point Source Parameters

Parameter Value Notes
Event Name La Habra
Origin Time 2014/03/29 04:09:42.97 Source: En-Jui
Origin Location -117.930; 33.922; 5.0km Source: En-Jui
Strike/Dip/Rake 1 134/55/155 Source: En-Jui, initial
Strike/Dip/Rake 2 239/70/38 Source: En-Jui, based on review of aftershock sequence
Rise Time 0.75 s
Origin X/Y EQ_lahabra_xy.list


SRC Format La Habra Source

  • MAGNITUDE = 5.12
  • FAULT_LENGTH = 5.0
  • FAULT_WIDTH = 2.25
  • DEPTH_TO_TOP = 4.7125
  • STRIKE = 239
  • RAKE = 38
  • DIP = 70
  • LAT_TOP_CENTER = 33.9119
  • LON_TOP_CENTER = -117.940
  • HYPO_ALONG_STK = 0.0
  • HYPO_DOWN_DIP = 1.125
  • DLEN = 0.1
  • DWID = 0.1

Volume

The four corners are:

  • -119.288842 34.120549
  • -118.354016 35.061096
  • -116.846030 34.025873
  • -117.780976 33.096503

And the box has size

  • 180,000 m x 135,000 m x 61,875 m

Runs

Hercules Runs

Run Number Etree Source Notes
1 ch-cvms400-100-4hz-200ms.e point-ricardo-134-55-155
2 ch-cvms426-223-4hz-200ms.e point-ricardo-134-55-155
3 ch-cvms400-100-4hz-200ms.e point-ricardo-239-70-38
4 ch-cvms426-223-4hz-200ms.e point-ricardo-239-70-38
5 ch-cvms400-100-4hz-200ms.e extended-ricardo
6 ch-cvms426-223-4hz-200ms.e extended-ricardo


BBP Run


La Habra Earthquake Observations

La Habra References


References

  1. Bielak, J., H. Karaoglu, and R. Taborda, 2011. Memory-efficient displacement-based internal friction for wave propagation simulation, Geophysics, 76(6):T131-T145.
  2. Taborda, R., Lopez, J., Karaoglu, H., Urbanic, J., and Bielak, J. (2010). Speeding up finite element wave propagation for large-scale earthquake simulations. Technical Report CMU-PDL-10-109, Carnegie Mellon University, Parallel Data Lab.
  3. Tu, T., Yu, H., Ramírez-Guzmán, L., Bielak, J., Ghattas, O., Ma, K.-L., & O’Hallaron, D.R., 2006. From mesh generation to scientific visualization: an end-to-end approach to parallel supercomputing, in Proceedings of the 2006 ACM/IEEE International Conference for High Performance Computing, Networking, Storage and Analysis, p. 15, IEEE Computer Society, Tampa, Florida.
Retrieved from "https://strike.scec.org/scecwiki/index.php?title=La_Habra_Simulations_on_Titan&oldid=10558"