What does tremor really look like? Initial results from an 84-element array with help from Seattle mafia Sweet, Ghosh, Creager, Houston, Pratt, …

Slides:



Advertisements
Similar presentations
Earth Science Mr. Bimber
Advertisements

IRIS’s Large N Initiative Hole, Seismic Instrumentation Technology Workshop, June2012 John Hole, Virginia Tech Chair of IRIS Large N Working Group SPATIAL.
A magnitude 7.1 struck early Saturday off Japan's east coast. The quake hit at 2:10 a.m. Tokyo time about 170 miles from Fukushima, and it was felt in.
Body and Surface Wave Seismic Tomography for Regional Geothermal Assessment of the Western Great Basin Glenn Biasi 1, Leiph Preston 2, and Ileana Tibuleac.
Moon Phases and eclipses.
Examine these primary sources of scientific evidence. What does this graph show about the extent and change in fires? Hint: click on thumbnail graph above.
Val Veirs Colorado College Colorado Springs, CO, Scott Veirs Beam Reach marine science and sustainability school Seattle, WA,
More cycles in the sky Announcements (no, not that kind)
Year 11 Tuesday March 3 rd To give information about exams, revision sessions and final practical exams. 2. To give some advice about revision.
Global Distribution of Crustal Material Inferred by Seismology Nozomu Takeuchi (ERI, Univ of Tokyo) (1)Importance of Directional Measurements from geophysicists’
Cold Sky Calibration Aquarius: D. M. Le Vine MWR: J. C. Gallo.
Spatial and Temporal Patterns of Deformation Through the Seismic Cycle Jeff Freymueller University of Alaska Fairbanks.
Recent ETS results in NW Washington Tremor Locations and Migration during last four ETS events Locked Zone relative to Tremor Location Inter ETS Tremor.
Earthquake Hazard Assessment in the Pacific Northwest: Site Response Thomas L. Pratt U. S. Geological Survey School of Oceanography University of Washington.
Very-Low-Frequency Earthquakes (VLFE) in SVI and Grid Moment-Tensor Inversion For details on GCMT inversion method, see Ito et al., GJI, 2006.
1 Virgo Commissioning progress and plans ILIAS, Jan 23 rd 2007 Matteo Barsuglia on behalf of the Commissioning Team.
An Earth Day Sidereal Day: 23 hr 56 min 4 sec Motion relative to background stars Mean Solar Day: 24 hours The average time between meridian crossings.
2-3 March 2009 Cascadia 2007 and Beyond Workshop, Seattle Results from Strainmeter Recordings of Cascadia “ETS” events Work by Evelyn Roeloffs, Wendy McCausland,
The Solar System.
Ms. Hartnett's Earth Science
A Look Inside the San Andreas fault at Parkfield Through Vertical Seismic Profiling Chavarria, Malin, Catchings, and Shalev Science, 302, pp ,
Planetary Science Round Earth / Flat Earth Planetary Science Vocabulary horizon - where sky and earth appear to meet line of sight - the straight unimpeded.
Astro Pages Earth and Space Science THE CYCLES OF THE MOON.
The Celestial Sphere The 88 official constellations cover the celestial sphere. If you do not have a model of the celestial sphere to bring to class, you.
The Earth-Moon-Sun System
A. Ghosh, EAS, Georgia Tech Distribution of b-value in the Middle America Trench, near Nicoya Peninsula, Costa Rica Abhijit Ghosh A. V. Newman, A. M. Thomas,
Industry-style combined active/passive dense array surveys: directions and issues. Dan Hollis, NodalSeismic, LLC 26 January 2014Active Source Workshop.
The Earth, The Sun, and The Moon
SCALES: PLANETARY. Andromeda Galaxy: 2 million light-years away Problem Problem for Astronomers: there is no sense of depth from looking at the sky. minutes.
Phase Retrieval Applied to Asteroid Silhouette Characterization by Stellar Occultation Russell Trahan & David Hyland JPL Foundry Meeting – April 21, 2014.
High Sensitivity Magnetic Gradiometer for Earthquake Research Applications ISRAEL 2005 Ivan Hrvoic H. Ginzburg, H. Zafrir, G. Steinitz, B. Shirman, G.
Keir Opie National Center for Transportation and Industrial Productivity (NCTIP) New Jersey Institute of Technology (NJIT) Paramics North American User.
New earthquake category Nature 447, (3 May 2007) | doi: /nature05780; Received 8 December 2006; Accepted 26 March A scaling law for slow.
Stars and galaxies. Constellations  Ancient Greeks, Romans and other cultures saw patterns of stars in the sky called constellations  They imagined.
Earth Science 22.2A Earth-Sun System
Updating Models of Earthquake Recurrence and Rupture Geometry of the Cascadia Subduction Zone for UCERF3 and the National Seismic Hazard Maps Art Frankel.
Section 19.2– Seismic Waves and the Earth’s Interior
Episodic Tremor in the Alaska/Aleutian Subduction Zone Chloe Peterson, Douglas Christensen, and Steve McNutt Geophysical Institute, University of Alaska.
Constraints on Seismogenesis of Small Earthquakes from the Natural Earthquake Laboratory in South African Mines (NELSAM) Margaret S. Boettcher (USGS Mendenhall.
Observation of diffuse seismic waves at teleseismic distances
P-Wave and S-Wave Chart
Slow Slip Events v. Earthquakes Using geodetic data to estimate source parameters.
Seismic Arrays presented at the WORKSHOP High Quality Seismic Stations and Networks for Small Budgets Volcan, Panama March 2004by Jens Havskov, Department.
Reflection Lab What is the relationship between the angle in and the angle out for light on a mirror?
Models for Fault Behavior
Recognizing Reflected Tremor Phases: Guidance from Synthetic Seismograms Amanda Klaus ESS 522 – Geophysical Data Analysis Final Project June 10, 2010.
STUDY GUIDE Wave Properties, Interactions, and Sound Waves
Earthquakes & Tsunamis. Earthquakes are a shaking of the ground. Some are slight tremors that barely rock a cradle. Others are so violent they can tear.
ETS - Science and Hazard the argument for close monitoring November 2008 John Vidale with input from Gomberg, Peng, Creager, Malone, Pratt, Houston, …
Astronomic Distances. Solar system- planets and other objects like comets and asteroids that travel around the sun Background.
Analysis of regional infrasound signals at IMS infrasound array in Mongolia a RCAG/MAS P.O.B-152, Ulaanbaatar-51Mongolia b CEA/DASE BP12, Bruyeres-le-Chatel,
Nanoseismic Monitoring by Seismic Navigation System (SNS) M. Joswig Institut für Geophysik, Universität Stuttgart, Germany data logger 3-D 1-D.
Ch Stars Part 1 Chapter 19, Section 1. Stars Stars are huge, hot, brilliant balls of gas. To learn about stars, scientists study starlight.
8K Light 8K Light Travelling light Bending and reflecting Colours.
Epicenter Hunt “The Game”
學生: 花翊筑 Alice Hua 指導老師: 陳卉瑄 教授 Kate Huihsuan Chen
4 min of arrival difference = 2,600 km
Université Joseph Fourier Grenoble, France
Wells, Nevada Earthquake February 21, 2008
One light year is equal to the distance traveled by light in one year (through empty space). One light year = 1 ly = 6 trillion miles = 9.5 trillion.
MAP ELEMENTS LINK.
Creager, Wech, Vidale, Melbourne
When does the P wave arrive? 08:08:00
Earthquakes.
Creager, Wech, Vidale, Melbourne
Creager, Wech, Vidale, Melbourne
Ken Creager, Wendy McClausland and Steve Malone
8.1 & 8.2 Mini Quiz (20 pts).
Light and Shadows Objective : To investigate the effect of distance between the object and the light source.
Bellringer Vocab Quiz TODAY!!!! Test Wednesday Direction
Presentation transcript:

What does tremor really look like? Initial results from an 84-element array with help from Seattle mafia Sweet, Ghosh, Creager, Houston, Pratt, …

Talk outline BackgroundBackground 2008 Pilot Array2008 Pilot Array Some irritating noisesSome irritating noises Geophysical noisesGeophysical noises Next step - Array of ArraysNext step - Array of Arrays

State of affairs What is tremor? What is tremor? –we don’t know physical process Can it tell us about updip great earthquakes? Can it tell us about updip great earthquakes? –Maybe defines edge of locked zone –Maybe loads megathrust at an unsteady rate

4 ETS Every 14 months Creager & Wech, U33A-0022 and 0026 * BS Array

5 84 sensors in a km 2, Caught 8 days with light tremor in March, then 17 days of heavy tremor passing directly underneath this May Time (days) UW dense array pilot study 1 km

6 Near and north Just daytime Downtown Seattle buzzer ? ~5Hz persistent sources for 8 days in March tremor LFEs storm tremor

7 Near and north Narrowband vibration Shallow angle of incidence Migrating direction Time progression on regional seismometers Boat noise Theoretical optimum

8 BS Array recorded in March most of a small, weak episode under Bremerton, some distance away. Detected 2180 minutes vs 539 minutes of tremor. Like earthquakes, no apparent minimum size. Storms Sensitivity compared to envelope method Sweet, U33A-0024

9 La Rocca, Science, in revision Checking location thrice S-P time Beam (rainbow) and envelope (green stars)

10 Movie of 14 hours of tremor Pink circles - peak of beam slownesses Rainbow background - entire beam Green stars - envelope location estimates Each mark shrinks then disappears with 30 minutes

11 Abhi Ghosh, last week Tremor more irregular than previously mapped? Tremor looks pointillist, more continuous, no evidence of large source volume so far.

12 EarthScope Array of Arrays experiment Volunteers? Contact –Justin Sweet –Abhijit Ghosh –Ken Creager –Heidi Houston Summer 2009 Summer 2010 Pitch for more grad student applications

13 The end Main points –Arrays give detailed recording of tremor –Traditional methods only recorded strongest tremor –Tremor source region looks patchy, pointillist