Research opportunities using IRIS and other seismic data resources John Taber, Incorporated Research Institutions for Seismology Michael Wysession, Washington.

Slides:



Advertisements
Similar presentations
Magnitude 7.1 NEAR THE EAST COAST OF HONSHU, JAPAN Thursday, April 7, 2011 at 14:32:41 UTC Japan was rattled by a strong aftershock and tsunami warning.
Advertisements

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.
A magnitude 2.9 earthquake occurred in the East Midlands region of the United Kingdom on 18 January The earthquake occurred at a depth of 13 km (8.
Prague, March 18, 2005Antonio Emolo1 Seismic Hazard Assessment for a Characteristic Earthquake Scenario: Integrating Probabilistic and Deterministic Approaches.
Interpreting Seismograms
Earthquakes.
Exploring Planet Earth Updated October 2011 The AS-1 Seismometer and AmaSeis Software – An Effective Educational.
A magnitude 7.3 earthquake occurred to the east of Kathmandu, in an area close to Mount Everest. This large earthquake is the largest aftershock so far.
Science for Planet Earth April 2010 A Decade of Earthquake Monitoring with an Educational Seismograph Larry.
A New Approach To Paleoseismic Event Correlation Glenn Biasi and Ray Weldon University of Nevada Reno Acknowledgments: Tom Fumal, Kate Scharer, SCEC and.
Seismic/Eruption Teaching Modules Lawrence W. Braile Sheryl J. Braile Teaching About Earthquakes.
STUDYING NEOTECTONICS WITH PLATE MOTION, SEISMOLOGICAL & GPS DATA: THEORY & PRACTICE Seth Stein, Northwestern University.
EARTHQUAKES AND TSUNAMI IN HAWAI‘I (GG103) ~50 years of Hawai‘i seismicity.
Locating the source of earthquakes Focus - the place within Earth where earthquake waves originate Epicenter on an earthquake– location on the surface.
Seismic/Eruption Lawrence W. Braile Using the Seismic/Eruption Program in Teaching Larry Braile IRIS GSA Earthquake.
Time-dependent seismic hazard maps for the New Madrid seismic zone and Charleston, South Carolina areas James Hebden Seth Stein Department of Earth and.
1.Intro to geology 2.Plate tectonics 3.Minerals 4.Rocks 5.Igneous rocks 6.Volcanism 7.Weathering & erosion 8.Sediments and Sedimentary rocks 9.Metamorphic.
Learning objectives Understand the relationship of earthquakes to faulting Familiarization with earthquake & wave (energy) terminology Understand the.
1 What is the Richter Scale? How large is a large earthquake? How is earthquake size measured? Earthquake Magnitude Module LRW-1 Prepared for SSAC by Laura.
2007 NSTA: St. Louis, Missouri Earthquake Prediction and Forecasting: A Case Study of the San Andreas and New Madrid Faults Sponsored by: IRIS (Incorporated.
Earthquake Focal Mechanisms
Earthquakes Susan Bilek Associate Professor of Geophysics New Mexico Tech How to figure out the who, what, where, why… (or the location, size, type)
Earthquakes.
Earthquakes – Comp. Sci Forces in Earth’s Crust
Earthquakes.
Earthquake Review.
Earthquakes (Chapter 8)
During the semester Introductions Basics of earthquakes History and Recording Damaging earthquakes and understanding seismic exposure Undertake loss assessment.
IRIS Data Tools and Animations John Taber, Tammy Bravo, Michael Hubenthal, Jenda Johnson.
Seismic Hazard Assessment for the Kingdom of Saudi Arabia
Crust and upper mantle structure of Tien Shan Orogen and its surroundings by ambient noise tomography and earthquake tomography Yong Zheng a, Yingjie Yang.
Web.ics.purdue.edu/~braile Online Searches
Earthquakes, log relationships, trig functions tom.h.wilson Department of Geology and Geography West Virginia University Morgantown,
Sharon Peters Michael Wells Castle Point on Hudson Hoboken, NJ (201)
Geology Flash Cards Grade 3 January 2015
An Introduction to Seismic Eruption software and an associated classroom activity Michael Hubenthal, IRIS Educational Specialist.
Using IRIS and other seismic data resources in the classroom John Taber, Incorporated Research Institutions for Seismology.
Earthquake forecasting using earthquake catalogs.
Earthquake hazard isn’t a physical thing we measure. It's something mapmakers define and then use computer programs to predict. To decide how much to believe.
Some Thoughts on IMW And Opportunity We represent a big area of the ANSS national program Bob Smith Univ. of Utah.
Accessing and using event data in the classroom Michael Hubenthal, IRIS Educational Specialist.
Earthquakes Ch. 15 Lesson 1. What are Earthquakes? Earthquakes are the vibrations in the ground that result from the movement along breaks in Earth’s.
Large Earthquake Rapid Finite Rupture Model Products Thorne Lay (UCSC) USGS/IRIS/NSF International Workshop on the Utilization of Seismographic Networks.
California Project Seismicity in the oil and gas fields Tayeb A. Tafti University of Southern California July 2, 2013.
GLOBAL EARTHQUAKE FORECASTS Yan Y. Kagan and David D. Jackson Department of Earth and Space Sciences, University of California Los Angeles Abstract We.
Yan Y. Kagan Dept. Earth and Space Sciences, UCLA, Los Angeles, CA ,
Learning Teams Red - Favorite hobbies Green - Favorite place on earth Blue – Teaching situation (Grade level, courses, etc) Yellow – Favorite activity.
Ground Deformation: Faulting and Folding Earthquakes and Mountain- Building.
Earthquakes and Earth’s Interior Key Points are Green.
Earthquakes.
Table of Contents Forces in Earth’s Crust Earthquakes and Seismic Waves Monitoring Earthquakes Earthquakes.
A 7.2 magnitude earthquake occurred about 250 km ENE of Kurli’sk, Russia. The earthquake occurred at a depth of km (76 miles). There are currently.
A magnitude 7.6 earthquake struck near the Solomon Islands on Sunday morning local time; there were no immediate reports of damage. The earthquake was.
7 th Grade – Chapter 7. stress tension compression shearing normal fault reverse fault strike-slip fault plateau earthquake focus epicenter P wave S wave.
Bellringer# 27 What is the Richter Scale? What is the greatest magnitude on the Richter scale? Where would an earthquake with the greatest magnitude be.
Understanding Earth Sixth Edition Chapter 13: EARTHQUAKES © 2011 by W. H. Freeman and Company Grotzinger Jordan.
Earthquakes. What are earthquakes? Vibration in the ground that result from movement along faults. Fault = a break in Earth’s lithosphere where one block.
Waves That Travel Through the Earth Mr. Keyes Layers of the Earth.
Introduction to seismology Mathilde B. Sørensen and Jens Havskov.
Earthquakes and tsunamis in the last week
Images courtesy of Google Earth (top), and USGS (bottom).
Images courtesy of Google Earth
Images courtesy of Google Earth (top), and USGS (bottom).
Ground Deformation: Faulting and Folding Earthquakes and Mountain- Building.
IRIS Seismographs in Schools Program
Understanding Earth Chapter 13: EARTHQUAKES Grotzinger • Jordan
Earthquakes & Plate Tectonics
Earthquake Machine, part 2
UNIT 4 The theory of plate tectonics explains Earth’s geological processes
Seismic Eruption - forecasting future earthquakes
Presentation transcript:

Research opportunities using IRIS and other seismic data resources John Taber, Incorporated Research Institutions for Seismology Michael Wysession, Washington University

Overview Hands on – Estimating seismic hazard using IRIS Earthquake Browser Discovering a predictive mathematical model Demo – Exploring regional tectonics using focal mechanisms – Recording and analyzing data from an educational or research-grade seismometer – Viewing a set of seismograms from an earthquake – USArray ground motion visualizations – Understanding earthquakes via a simple physical model

Estimating seismic hazard Research problem You and your partner have been asked to compare the seismic hazard in two regions to determine which is safer for building a new manufacturing plant. 1.What type of data would you need to collect to make the comparison? 2. How could you express your findings in a quantitative way?

Earthquake hazard from a single fault Would like to know How often do the biggest earthquakes occur? When will the next big one occur? Extend earthquake history with geologic record

Earthquake recurrence along a single fault Sieh et al., 1989 With a partner: Determine when the next Pallett Creek earthquake is going to occur. Can you estimate the uncertainty in your answer?

Earthquake recurrence along a single fault can be highly variable: probabilities hard to assess M >7: mean = 132 yr Standard deviation = 105 yr Estimated probability of next earthquake in 30 yrs is 7-51% -> Nearly Random! Sieh et al., 1989

How can we deal with unpredictable nature of individual faults? Try regional approach Use the rate of earthquake occurrence in one time period to forecast earthquake activity in another time period Combine results from multiple faults Consider more than just the biggest earthquakes

IRIS Earthquake Browser -

Can use for introduction to plate tectonics – Explore plate boundaries – Turn plate boundary lines on and off – Interactive 3D viewer General exploration of spatial distribution of local and regional seismicity

Estimating seismic hazard Steps: Select a region of the world that is of interest to you Interrogate the earthquake catalog to determine the number of events that occur in a 25 year period – Set the Time Range – Set the Magnitude Range In an Excel spreadsheet, record the total number of events for each magnitude range Determine the number of earthquakes/year for each magnitude range Plot the magnitude range vs the number of earthquakes/year

IRIS Earthquake Browser -

Questions to discuss with a partner Given the range of the data, what sort of plot gives the clearest representation of the data? Do you see any patterns or trends in your data? How does your plot compare to your partner’s plot of a different region? What is the likelihood of earthquakes of magnitude 6.0 or greater and 7.0 or greater occurring in the next year in the 2 regions? What is the likelihood of these events occurring in the next 100 years in each region?

Earthquakes, Magnitude >3.5,

Earthquakes/year Magnitude California (blue) and Eastern US Earthquakes (red)

How often does a M6 earthquake occur?

How often does a M7 earthquake occur?

Real, imperfect data set

Interpretation questions How can you use the seismicity information to estimate which of your two regions would be a safer choice for the manufacturing plant mentioned at the beginning of the exercise? What are some assumptions, limitations, and potential sources of error in drawing conclusions about long-term seismic hazard using the above technique?

Ground shaking from a magnitude 5 earthquake in the east is approximately equivalent to that of a magnitude 6 earthquake in the west. Virginia M 5.8 California 6.5 Going from seismicity rate to ground shaking

USGS National Seismic Hazard Map Submitted draft exercise explores hazard map

Exploring regional tectonics using f o c a l m e c h a n i s m s Visual sorting of normal, reverse, and strike-slip mechanisms Can explore distribution in a subduction zone IRIS main menu: Data and Software > Products – Select Moment Tensors, then Quick links – Focal mechanism animation available

Recording and analyzing seismic data u s i n g j A m a s e i s Real time data streaming and simple analysis – Simple filtering, arrival picking, locations, magnitudes

Recording and analyzing seismic data u s i n g j A m a s e i s Real time data streaming and simple analysis – Simple filtering, arrival picking, locations, magnitudes Up to 3 data streams can be viewed and stored locally – Local or remote educational seismographs – Any global research station received and stored in the IRIS Data Management Center

Recordings from the Global Seismic Network Real time data streaming and simple analysis

Potential seismograph-related research t o p i c s Local seismograph calibration and sensitivity – Distance/magnitude relationship Alan Kafka – Analyzing seismic data to find what earthquakes were recorded and then learning about the tectonics of each region Dave Voorhees’ student – Finding the best recording location

Rapid E a r t h q u a k e V i e w e r Developed and maintained by Univ S. Carolina

Understanding earthquakes via a simple p h y s i c a l m o d e l Earthquake machine Simple data collection and analysis leads to very similar result to real earthquake catalog

USArray Ground Motion Visualizations Visualizations exist for all parts of lower 48 1D and 3D versions

EPO web p a g e f r o m w w w. i r i s. e d u Feedback? Comments? Questions?

EXTRAS

USArray Ground Motion Visualizations Visualizations exist for all parts of lower 48

Investigating Earth structure using t o m o g r a p h i c m o d e l s Select a region and a submitted velocity model and generate a cross section Fate of slabs Crustal and upper mantle thickness under mountain ranges

Selection from focal mechanism animation