39
Sri Lanka Earthquake & Tsunami Warning Training Program Sri Lanka Earthquake & Tsunami Warning Training Sri Lanka Earthquake & Tsunami Warning Training Program Program Session III.3 Global and Local Arrays April 5, 2006 CETRAC, Sri Lanka

Sri Lanka Earthquake & Tsunami Warning Training Program

  • Upload
    herbst

  • View
    30

  • Download
    1

Embed Size (px)

DESCRIPTION

Sri Lanka Earthquake & Tsunami Warning Training Program. Session III.3 Global and Local Arrays April 5, 2006 CETRAC, Sri Lanka. Topics covered:. Types of seismic arrays How arrays are used Example global networks. Seismic array :. Has common time base (one clock) - PowerPoint PPT Presentation

Citation preview

Page 1: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training ProgramSri Lanka Earthquake & Tsunami Warning Training ProgramSri Lanka Earthquake & Tsunami Warning Training Program

Session III.3

Global and Local Arrays

April 5, 2006

CETRAC, Sri Lanka

Page 2: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Topics covered:

Types of seismic arrays How arrays are used Example global networks

Page 3: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Seismic array:

Has common time base (one clock) Has common recording center Waves remain coherent as they

propagate across the array

Page 4: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

An array can be used as an antenna to determine the direction from which the seismic waves arrive. This process, called beamforming, tells where the earthquake is located.

Page 5: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Seismic network:

Each station’s clock is independent Data recording may be at the station

or at a common data center Waves may not be coherent as they

propagate across the network

Page 6: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

In a network, the location of an earthquake is found by triangulation. Information from all stations is used.

Page 7: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

High frequency waves attenuate (damp out) rapidly with distance. Low frequency waves diminish in amplitude more slowly with distance traveled.

The Earth acts like a filter!

Page 8: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

IRIS GSN SYSTEME

QU

IVA

LEN

T E

AR

TH P

EA

K A

CC

ELE

RA

TIO

N (

20 L

OG

M/S

EC

2 )

PERIOD (SECONDS)

Global networks choose instruments capable of recording long period waves. Local arrays may use short period sensors to record local earthquakes.

Page 9: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

The 2004 Sumatra-Andaman Isl quake radiated very long period seismic waves that were recorded by global networks.

Page 10: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

IRIS/USGS GLOBAL NETWORK

- USGS Albuquerque Seismological Laboratory- IRIS/IDA Group at IGPP, Scripps Institution of Oceanography

University of California, San Diego- University Networks and Affiliates

Page 11: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

GSN Goals:

develop high quality seismic data acquisition equipment

• deploy systems globally at 2000 km spacing

• make data openly available to all who request a copy

Page 12: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

GSN data are used to study the internal seismic structure of the Earth:

Courtesy of Adam Dziewonski, Harvard University

Page 13: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Page 14: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Page 15: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

German GEOFON Network

Page 16: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

French GEOSCOPE Network

Page 17: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Japan FNET

Page 18: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Chinese Digital Seismic Stations

Page 19: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Page 20: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Operational Planned

Courtesy L. Kong

Page 21: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

A design for Sri Lanka:

Use local stations to locate earthquakes in or near Sri Lanka

• Use global network data (from Internet) to locate major earthquakes distant from Sri Lanka

Page 22: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

A note on noise at seismic stations.

The quietest stations in the world are on continents.

Page 23: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Stations near the ocean are noisier.

Page 24: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

This peak is caused by ocean waves breaking on coastlines.

Page 25: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

This peak is caused by ocean waves also.

Page 26: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

An important source of long period noise is changes in air pressure.

Page 27: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

If possible, locate seismic stations away from the coast where noise conditions are better (noise is lower).

Page 28: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Another important subject…

Remember the DAS?

Page 29: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Other equipment needed:

Clock to time the data “DAS” to convert electric current

to numbers for a computer to process

Page 30: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

The DAS converts electrical current from the seismometer into numbers to be processed by the conputer.

The electrical current from the seismometer is continuous, but the DAS produces numbers only at set intervals of time, the digitization rate. The DAS bundles these numbers into a packet called a data record.

Page 31: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

The DAS converts electrical current into numbers.

Page 32: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

How the DAS bundles the data depends upon the computer programs running inside the DAS.Some DASs produce a record containing data for a fixed period of time. Other DASs produce a record of a fixed size. In this case, the period of time contained varies from record to record because the data are compressed.

Page 33: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

This “seismogram” is very simple:

Page 34: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

We “compress” 20 numbers into 3 (a, b, c):

X = a T2 + bT + c

Page 35: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Data records are passed from computer to computer using data telemetry methods. Data centers may pass data to computers from other organizations. By sharing data, both organizations obtain more information.

Page 36: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

Data center software is quite complex. Several packages exist, including this commercial one.

Page 37: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

NRTS_utilities: a simple IDA display program

Page 38: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

You can display data from PALK and other stations

Page 39: Sri Lanka Earthquake & Tsunami Warning Training Program

Sri Lanka Earthquake & Tsunami Warning Training Program

The buttons at the top control the display