Earthquake Magnitude Calculator for the AS-1 Seismograph 1



Similar documents
Name: Date: Class: Finding Epicenters and Measuring Magnitudes Worksheet

SUMMARY OF MAGNITUDE WORKING GROUP RECOMMENDATIONS ON DETERMINING EARTHQUAKE MAGNITUDES FROM DIGITAL DATA

Locating the Epicenter and Determining the Magnitude of an Earthquake

Plotting Earthquake Epicenters an activity for seismic discovery

The earthquake source

EARTHQUAKES. Compressional Tensional Slip-strike

Real-Time Seismic Image Display IRIS Seismographs in Schools Program

Unit 4 Lesson 6 Measuring Earthquake Waves. Copyright Houghton Mifflin Harcourt Publishing Company

Seismic Waves Practice

Earthquake Lab. A. Locate the Epicenter. Name: Lab Section:

Earthquake Magnitude

FOURTH GRADE EARTHQUAKES 1 WEEK LESSON PLANS AND ACTIVITIES

Introduction to Seismology Spring 2008

Name Date Class. By studying the Vocabulary and Notes listed for each section below, you can gain a better understanding of this chapter.

Earthquakes, faulting, beach-balls, magnitude scales

Boston College. The Graduate School of Arts and Sciences. Department of Geology and Geophysics

Determination of source parameters from seismic spectra

Earthquakes. Earthquakes: Big Ideas. Earthquakes

Earthquakes.

Earthquakes. Seismograph stations operated by the British Geological Survey

THE 2004 SUMATRA EARTHQUAKE AND INDIAN OCEAN TSUNAMI: WHAT HAPPENED AND WHY

Magnitude 7.2 GUERRERO, MEXICO

Activity #1-HS What is a Seismometer? High School Level

Earthquakes, volcanoes and plate tectonics in ArcGIS Online

DYNAMIC CRUST: Unit 4 Exam Plate Tectonics and Earthquakes

Geology 112 Earthquakes. Activity 1 Worksheet Introduction to the Course. What is a Fault? What is an Earthquake?

Real time earthquake monitoring for early warning of tsunamis

NATURAL DISASTERS Vol. I - Earthquake Parameters Including Strong Earthquakes- S.L.Yunga EARTHQUAKE PARAMETERS INCLUDING STRONG EARTHQUAKES

Mapping the Tyrrhenian and Adriatic Mohos across the northern and central Apennine chain through teleseismic receiver functions

How do scientists measure earthquakes?

Bandwidth-dependent transformation of noise data from frequency into time domain and vice versa

Lecture 12 Earthquake Magnitude

Building 1D reference velocity model of the Irpinia region (Southern Apennines): microearthquakes locations and focal mechanism

The Dynamic Crust 2) EVIDENCE FOR CRUSTAL MOVEMENT

Chapter 5: Earthquakes

Data Analysis and Seismogram Interpretation

Welcome to Vibrationdata

FA21 Installation & User Guide Version 5.16

Seismographs. Lesson 7. Seismographs recording activity on Kilauea

Seismic Observations during September 11, 2001, Terrorist Attack

Magnitude 8.8 OFFSHORE MAULE, CHILE

1 Introduction. External Grant Award Number: 04HQGR0038. Title: Retrieval of high-resolution kinematic source parameters for large earthquakes

Data in seismology: networks, instruments, current problems

Operate Backup Data. This how-to document will walk you through how to acquire and view your (M)SDS collection from the backup we send you.

Guidance for IA DMM: Connecting Your Computer to FSU Video File Server

CLIMWAT 2.0 for CROPWAT

EARTHQUAKE MAGNITUDE

SMIP2000 Seminar Proceedings COSMOS VIRTUAL STRONG MOTION DATA CENTER. Ralph Archuleta

The Severity of an Earthquake U.S. Department of the Interior/Geological Survey

ARIS Education Package Process Design & Analysis Installation Guide. Version 7.2. Installation Guide

Zanibal Plug-in For Microsoft Outlook Installation & User Guide Version 1.1

Building a simple seismometer

Exploring plate motion and deformation in California with GPS

Geology for Engineers Earthquakes

Observed Characteristics of Regional Seismic Phases and Implications for P/S Discrimination in the European Arctic

National Site Tracking System

Setting up VMware ESXi for 2X VirtualDesktopServer Manual

On Es-spread effects in the ionosphere connected to earthquakes

Office of Public and Indian Housing PIH Information Center (PIC)

Surface sediment effects on teleseismic P wave amplitude

About WINZIP : Basic User Guide

Using Internet or Windows Explorer to Upload Your Site

Geological Maps 3: Faulted Strata

Reading GPS Time Series Plots Worksheet

3D Visualization of Seismic Activity Associated with the Nazca and South American Plate Subduction Zone (Along Southwestern Chile) Using RockWorks

Regents Questions: Plate Tectonics

AssetGen Desktop Professional Download and Installation Instructions

Earthquake Focal Parameters and Lithospheric Structure of the Anatolian Plateau from Complete Regional Waveform Modeling

Exclaimer Mail Archiver WebApp Guide IT SERVICES. University of Sunderland

Design Example 1 Design Spectral Response Acceleration Parameters 11.4

Seismic waveform data retrieval

Where in the World Are All the Earthquakes?

ABSG Consulting, Tokyo, Japan 2. Professor, Kogakuin University, Tokyo, Japan 3

UrEDAS, URGENT EARTHQUAKE DETECTION AND ALARM SYSTEM, NOW AND FUTURE

DESIGN A WEB SITE USING PUBLISHER Before you begin, plan your Web site

Chapter 6 Plate Tectonics and Earthquakes

Networks, instruments and data centres: what does your seismic (meta-) data really mean? Joachim Wassermann (LMU Munich)

Installing and Configuring Microsoft Dynamics Outlook Plugin to Use with ipipeline MS CRM

MDM Mass Configuration Tool User s Manual

Windows XP with Symantec AntiVirus 10 Corporate Edition

Curriculum Map Earth Science - High School

Frequency Response of Filters

FREE FALL. Introduction. Reference Young and Freedman, University Physics, 12 th Edition: Chapter 2, section 2.5

Bridging People and Process. Bridging People and Process. Bridging People and Process. Bridging People and Process

Simulating Aftershocks for an On Site Inspection (OSI) Exercise

SOFTWARE FOR GENERATION OF SPECTRUM COMPATIBLE TIME HISTORY

LT Auditor+ for Windows

A New Look at an Old Tool the Cumulative Spectral Power of Fast-Fourier Transform Analysis

Earthquakes Natural and Induced. Rick Aster Professor of Geophysics and Department Head Geosciences Department Colorado State University

TRAINING SYSTEM AND INFORMATION NETWORK FOR EARTHQUAKE DISASTER MITIGATION

Studying Topography, Orographic Rainfall, and Ecosystems (STORE)

Technote 20 Using MSIE to FTP into an AcquiSuite

Installing and using the driver

Using Remotely Sensed Data From ASTER to Look Impact of Recent Earth Quakes in Gujarat, India.

Suggestions and Tips for Managing and Uploading Files for the AEP Application

Transcription:

Magnitude calculator for the AS-1 Page 1 of 23 Earthquake Magnitude Calculator for the AS-1 Seismograph 1 Lawrence W. Braile and Saptarshi Dasgupta, Purdue University SKIP TO CALCULATORS Introduction: Magnitude is an estimate of the energy release or size of an earthquake. The estimates are calculated from the amplitude of wave energy on a seismograph adjusting for the magnification of the seismograph and the distance of the seismograph station from the earthquake. Click here for more details and examples of magnitude calculation using the AS-1 seismograph. A detailed discussion about the different kinds of magnitudes can be found at the USGS site. 1 Last modified November 11, 2004 The web page for this document is: http://web.ics.purdue.edu/~braile/edumod/magcalc/magcalc.htm. The URL for an MS Word version of this document is: http://web.ics.purdue.edu/~braile/edumod/magcalc/magcalcdoc.doc. Developed by Lawrence W. Braile and Saptarshi Dasgupta, Purdue University, May, 2003. Funding for this development provided by IRIS and the National Science Foundation. Copyright 2003-4. L. Braile. Permission granted for reproduction for non-commercial uses.

Magnitude calculator for the AS-1 Page 2 of 23 This earthquake magnitude calculator is designed for the AS-1 Seismograph. Specifications of the instrument can be found at web.ics.purdue.edu/~braile/edumod/as1mag/as1mag.htm. The description and examples presented here are for the AS-1 vertical component seismograph and the AmaSeis Software. The AmaSeis program connects the AS-1 seismograph to a computer running Windows, provides a continuous seismic record on the monitor, and includes several display and analysis tools. The seismograph records shown here were recorded using an AS-1 seismograph at West Lafayette, IN (Latitude 40.484 N, Longitude 86.881 W). Results of earthquake monitoring with an AS-1 seismograph and AmaSeis software, including epicenter-to-station distance calculations from S- P times and magnitude calculations, are illustrated at: web.ics.purdue.edu/~braile/edumod/magcalc/as1results.htm.

Magnitude calculator for the AS-1 Page 3 of 23 AS-1 Seismometer Things to know before using the Calculator: The calculator needs three inputs to measure the desired magnitude. The user must supply the Amplitude (in digital units; this amplitude is converted by the calculator to microns of ground displacement using seismometer characteristics determined by calibration of the seismometer), the Period (in seconds) and the Distance (in degrees, geocentric angle). The terms are briefly explained here. For more details, please visit the links shown above. Epicentral Distance vs. Surface Distance

Magnitude calculator for the AS-1 Page 4 of 23 Click on the type of Magnitude to calculate: Body Wave Magnitude (mb) Surface Wave Magnitude (MS) mblg Magnitude - (1) 0.5 < D < 4 (2) 4 <= D <30 (D=Distance in degrees) Last modified March 14, 2006 Download an MS Word version of the entire AS-1 Magnitude Calculator document Download a folder (~2.4MB) that contains a version of the AS-1 Magnitude Calculator that can be run locally on your computer. Last modified October 14, 2003. The download files will be called MagCalcLocal.exe.zip. It is a self-extracting executable file. Double click to open and unzip (of you don't have a zip program, go to www.winzip.com where you can download a free evaluation version). A folder called MagCalcLocal will be created. After placing this folder on your desktop and opening the folder, double click on MagCalc.htm and you will be able to perform all the magnitude calculations without being connected to the Internet. Of course to access links that are to Internet locations, you will need to be connected. The folder also contains an MS Word file that includes the entire AS-1 Magnitude Calculator document (instructions and examples). Body Wave Magnitude (25 deg < D < 90 deg, T~1-3 s)

Magnitude calculator for the AS-1 Page 5 of 23 Fig. (a) AmaSeis 24-hr record showing the Iceland Earthquake. Fig. (b) Extracted seismogram for the Iceland earthquake showing the P wave and the surface waves. Fig. (c) Close-up of the P-wave arrival. Click on the image for an enlarged view and an example of the measuring the amplitude and period. Supply the first three inputs in the Calculator and click on <Calculate> to find the mb Magnitude. EARTHQUAKE MAGNITUDE Amplitude Distance Period Magnitude Calculate Digital Units From AS-1/AmaSeis Clear Degrees Seconds mb

Magnitude calculator for the AS-1 Page 6 of 23 mb = log10(a/t) + 0.01*D + 5.9 (Compressional Body Wave (P-wave) Magnitude) defined by Gutenberg and Richter (1956) except that T, the period in seconds, is restricted to 1 to 3 s and A, the ground amplitude in micrometers, is not necessarily the maximum in the P group. D, the epicentral distance should be in the range 25-90. Use only the following values of T : 1, 1.5, 2, 3, 5 seconds. Enlarged Views (Body Wave Magnitude) Fig. (a) AmaSeis 24-hr record (screen display) for the Iceland Earthquake.

Magnitude calculator for the AS-1 Page 7 of 23 Fig. (b) Extracted seismogram of the Iceland earthquake (6/21/2000) containing the P arrival and the surface wave arrivals. Fig. (c) Close-up of the P-wave arrival for the Iceland earthquake and example amplitude and period measurements.

Magnitude calculator for the AS-1 Page 8 of 23 Example: D = 44.23 degrees A = 48 digital units T = 2 seconds mb = 5.8 The official USGS mb magnitude is 6.1. Check to see that the calculator works with these values. Surface Wave Magnitude (20 deg < D < 160 deg, T~20 s) Fig. (a) AmaSeis 24-hr record of the August 4, 2000, MS 7.1 Sakhalin Island earthquake. Fig. (b) Extracted seismogram of the Sakhalin Island earthquake showing the P arrival and the surface wave arrivals. Fig. (c) Close-up of the surface wave arrivals. Click on the image for an enlarged view and an example of measuring the amplitude and period. Supply the first three inputs in the Calculator and click on <Calculate> to find the MS Magnitude.

Magnitude calculator for the AS-1 Page 9 of 23 EARTHQUAKE MAGNITUDE Amplitude Distance Period Magnitude Calculate Digital Units from AS-1/AmaSeis Clear Degrees Seconds MS Ms = log (A/T) + 1.66 log D + 3.3 where A is the maximum ground amplitude in micrometers (microns) of the vertical component of the surface wave within the period range 18 to 22 s. T is the period in seconds. Use T=20s for the calculator. D is the distance in geocentric degrees (station to epicenter) and 20 <= D <= 160. Enlarged Views (Surface Wave Magnitude) Fig. (a) AmaSeis 24-hr record showing the Sakhalin Island earthquake.

Magnitude calculator for the AS-1 Page 10 of 23 Fig. (b) Extracted seismogram for the Sakhalin Island earthquake (8/4/2000) showing the P wave and surface wave arrivals.

Magnitude calculator for the AS-1 Page 11 of 23 Fig. (c) Close-up of the Surface wave arrival for the Sakhalin Island earthquake and example amplitude and period measurements. Example: D = 81.08 degrees A = 48 digital units T = 20 seconds MS = 7.0 The official USGS MS magnitude is 7.1. Check to see that the calculator works with these values. mblg Magnitude (0.5 < D < 4, T~1 s)

Magnitude calculator for the AS-1 Page 12 of 23 Fig. (a) AmaSeis 24-hr record showing the June 18, 2002, mblg 5.3 Evansville earthquake. Fig. (b) Extracted seismogram showing the Lg waves. Fig. (c) Closeup of the Lg wave arrival. Supply the first three inputs in the Calculator and click on Calculate to find the mblg Magnitude. EARTHQUAKE MAGNITUDE Amplitude Distance Period Magnitude Calculate Digital Units From AS-1/AmaSeis Clear Degrees Seconds mblg mblg = 3.75 + 0.90 log D + log (A/T) for 0.5 <= D <= 4 (Body Wave Magnitude using the Lg wave) as proposed by Nuttli (1973) where A is the ground amplitude in micrometers and T is the period in seconds calculated from the vertical component 1-second Lg waves. Use only the following values of T: 1, 1.5, 2, 3 seconds. D is the distance in geocentric degrees. The mblg magnitude formula is primarily used for earthquakes at relatively small distance in intraplate regions such as central and eastern North America. Enlarged Views (mblg Magnitude, distance 0.5 o to 4 o )

Magnitude calculator for the AS-1 Page 13 of 23 Fig. (a) AmaSeis 24-hr record showing the Evansville earthquake.

Magnitude calculator for the AS-1 Page 14 of 23 Fig. (b) Extracted seismogram for the Evansville earthquake (6/18/2002) containing the P arrival and the Lg wave arrivals.

Magnitude calculator for the AS-1 Page 15 of 23 Fig. (c) Close-up of the Lg wave arrivals for the Evansville earthquake and example amplitude and period measurements. Example: D = 2.59 degrees A = 1250 digital units T = 2 seconds mblg = 5.0 The official USGS mblg magnitude is 5.3. Check to see that the calculator works with these values.

Magnitude calculator for the AS-1 Page 16 of 23 Lg Wave Magnitude (4 < D < 30, T~1 s) Fig. (a) AmaSeis 24-hr record showing the April 29, 2003, mblg 4.9 NE Alabama earthquake. Fig. (b) Extracted seismogram showing the Lg waves. Fig. (c) Close-up of the Lg wave arrival. Supply the first three inputs in the Calculator and click on Calculate to find the mblg Magnitude. EARTHQUAKE MAGNITUDE Amplitude Distance Period Magnitude Calculate Digital Units From AS-1/AmaSeis Clear Degrees Seconds mblg mblg = 3.30 + 1.66 log D + log (A/T) for 4 <= D <= 30 (Body Wave Magnitude using the Lg wave) as proposed by Nuttli (1973) where A is the ground amplitude in micrometers and T is the period in seconds calculated from the vertical component 1-second Lg waves. Use only the following values of T: 1,

Magnitude calculator for the AS-1 Page 17 of 23 1.5, 2, 3 seconds. D is the distance in geocentric degrees. The mblg magnitude formula is primarily used for earthquakes at relatively small distance in intraplate regions such as central and eastern North America. Enlarged Views (mblg Magnitude, distance 4 o to 30 o ) Fig. (a) AmaSeis 24-hr record showing the NE Alabama Earthquake.

Magnitude calculator for the AS-1 Page 18 of 23 Fig. (b) Extracted seismogram for the NE Alabama earthquake (4/29/2003) containing the P arrival and the Lg wave arrivals. Fig. (c) Close-up of the Lg wave arrivals for the NE Alabama earthquake and example amplitude and period measurements.

Magnitude calculator for the AS-1 Page 19 of 23 Example: D = 6.05 degrees A = 770 digital units T = 1.5 seconds mblg = 5.3 The official USGS mblg magnitude is 4.9. Check to see that the calculator works with these values. Using the AS-1 Seismograph and AmaSeis Software in the Classroom Recording Earthquakes, Calculating Magnitude and Epicenter to Station Distance Lawrence W. Braile, Purdue University, braile@purdue.edu, http://web.ics.purdue.edu/~braile 5 minutes January 22, 2003, M7.8, Colima, Mexico earthquake recorded on an AS-1 seismograph and AmaSeis software at West Lafayette, IN. Distance = 26.01 degrees. Seismogram was filtered from 0.001 0.1 Hz. Maintaining a catalog of recorded earthquakes is a convenient and educational exercise associated with educational seismograph operation. Data entries require observation and analysis of seismograms, retrieving information from the internet and performing simple calculations.

Magnitude calculator for the AS-1 Page 20 of 23 Continuous or short duration (several weeks or months) recording of earthquakes with an educational seismograph is an excellent component of an in-depth science experience that includes record keeping, mathematical calculations and opportunities for significant learning about earthquakes, seismology, plate tectonics and related Earth science. Using the seismograph and recorded seismograms, students can do science using their own real data rather than just reading about or listening to descriptions of science. Monitoring earthquakes requires the useful exercises of maintaining an instrument, good record keeping (see example of a portion of an earthquake catalog above), retrieving additional information on the earthquake from the Internet, and making consistent observations of data. Over 3 years of experience with monitoring earthquakes with the AS-1 seismograph demonstrates that even in the relatively low seismicity Midwest or eastern North America, frequent (mostly teleseismic) earthquakes are recorded at relatively quiet sites. Visible earthquake seismograms are present every few days and an event that produces a seismogram that can be used for magnitude or distance calculations occurs, on the average, about once per week. The AmaSeis software (developed by Alan Jones for the AS-1 seismograph with support from IRIS) is easy to use and provides several useful features and tools for archiving, viewing and analyzing data. Exercises that use the recorded earthquake data include determining magnitude and epicenter to station distance. Although the AS-1 is a relatively simple and inexpensive seismograph, the results of these analyses are reasonably accurate (see examples below) thus validating the students efforts and increasing the interest in learning. Additional information about the AS-1 seismograph, AS-1 magnitude calculations and using the AS-1/AmaSeis seismograph in educational seismology is contained in the listed website.

Magnitude calculator for the AS-1 Page 21 of 23 Using the AmaSeis travel time curve tool to determine the epicenter-to-station distance from the S-P arrival times. January 22, 2003, M7.8, Colima, Mexico earthquake recorded on an AS-1 seismograph and AmaSeis software at West Lafayette, IN; Distance = 26.01 degrees. Comparison of AS-1 S-P Distance and Calculated Distance 110 Estimated Distance (Degrees; from AS-1 S-P Times) 100 90 80 70 60 50 40 30 20 10 0 0 20 40 60 80 100 Calculated Distance (Degrees; from USGS epicenter) Comparing actual and AS-1/AmaSeis S-P calculated distances. N = 95; Standard Deviation = 2.29 degrees (April, 2006).

Magnitude calculator for the AS-1 Page 22 of 23 9 Comparison of AS-1 and USGS Magnitudes 8 7 AS-1 Magnitude 6 5 mb magnitudes MS magnitudes 4 mblg magnitudes 3 3 4 5 6 7 8 9 USGS (official) Magnitude Comparing actual and AS-1/AmaSeis magnitudes (April, 2006). The AS-1 magnitude calculations result in accurate magnitude determinations. Standard deviations of the differences between AS-1 (single station) and USGS (average of many stations) magnitudes are similar to other (standard seismograph) single station uncertainties. MS Magnitudes: N = 116; Standard Deviation = 0.25 magnitude units. mb Magnitudes: N = 229; Standard Deviation = 0.27 magnitude units. mblg Magnitudes: N = 27; Standard Deviation = 0.34 magnitude units.

Magnitude calculator for the AS-1 Page 23 of 23 Comparison of AS-1 (mblg, mb and MS) and USGS Mw Magnitudes 9 8 MS magnitudes AS-1 Magnitude 7 6 5 mb magnitudes 4 mblg magnitudes 3 3 4 5 6 7 8 9 USGS (official) Mw Magnitude Although we cannot calculate Moment Magnitudes (Mw or simply, M) from AS-1 seismograms, the mb, MS and mblg magnitudes calculated from AS-1 seismograms provide reasonably accurate estimates of Mw. This figure shows the comparison of AS-1 magnitudes (mblg, mb and MS) with USGS Mw magnitudes. Return to L. Braile s Home Page