1. A
SEMINAR PRESENTATION
ON
“tsunami
warning system”
2013-2014
SUBMITTED TO:
SUBMITTED BY:
Mr. Amit Kumar Prajapati
Mr. Rajveer Marwal
Seminar Coordinators (Sec B)
Vibhor Rathi
4th Year, 8th Sem.
EC/10/148
DEPARTMENT OF ELECTRONICS & COMMUNICATION ENGINEERING
POORNIMA COLLEGE OF ENGINEERING, JAIPUR
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2. CONTENTS
Tsunami
Tsunami Warning System
Detecting Tsunami
Seismometers
Tidal Gauge
DART Buoys
Digiquartz Broadband Depth Sensor
Acoustic Transducer
Acoustic Link
DART I & II System
Advantages & Disadvantages
Future Scope
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3. TSUNAMI
It is a series of wave with long wavelength and long wave
period.
Apart from seismic activity, there are many other factors
responsible for Tsunami.
These gigantic waves are probably one of the most
powerful and destructive forces of nature.
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4. TSUNAMI WARNING SYSTEM
TWS is a system which detects tsunami and issue a
warning to prevent loss of life and property.
This system consist of two main parts:
TWS
Network of
sensors
Communication
Infrastructure
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5. WORKING OF TWS
Network of seismic monitoring station at sea floor
detects presence of earthquake.
Seismic monitoring station determines location and
depth of earthquake having potential to cause tsunami.
Any resulting tsunami are verified by sea level
monitoring station such as DART buoys, tidal gauge.
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6. TYPES OF TWS
There are two distinct types of TWS:
TWS
International
Warning
System
National
Warning System
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7. INTERNATIONAL WARNING SYSTEM
This system uses both data like seismic and water level
data from coastal buoys.
Tsunami travel at 500-1000 km/hr, while seismic wave
travel at 14,400 km/hr.
This give sufficient time for tsunami forecast to be
made.
It is commonly used in Pacific ocean and Indian ocean.
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8. NATIONAL WARNING SYSTEM
This system use seismic data about nearby recent
earthquake.
This system is unable to predict which earthquake will
produce significant tsunami.
NWS
Tsunami
Watches
Tsunami
Warning
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9. TSUNAMI WATCH
Watch is issued based on seismic information.
Watch is issued without confirmation that destructive
tsunami is underway.
Tsunami watch is issued to officials which may later
impact the watch area.
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10. TSUNAMI WARNING
Tsunami warning is issued when potential tsunami is
expected.
It alert officials to take action for entire tsunami hazard
zone.
Warning is issued automatically if an earthquake
powerful enough to create tsunami occur nearby.
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12. DETECTING TSUNAMI
Three types of technologies are used for detecting
tsunami:
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2
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• SEISMOMETERS
• COAST TIDAL GAUGES
• DART BUOYS
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13. SEISMOMETERS
Information available about source of tsunami is based
on seismic information.
Earthquake are measured based on its magnitude
recorded by its seismograph.
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14. DRAWBACK OF SEISMOMETERS
Data are indirect and interpretation is difficult.
It involve poor understanding of seismic coupling.
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15. TIDAL GAUGE
Measure sea level near coastal area.
Continuously monitors and confirms tsunami waves
following an earthquake.
If tsunami occurred other than earthquake we depend
solely on data of tidal gauge.
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16. DRAWBACK OF TIDAL GAUGE
May not survive impact of tsunami.
Cannot provide data that are especially important to
operational hazard assessment directly.
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17. DART BUOYS
Report to tsunami warning centre, when tsunami occur.
Information are processed to produce a new and more
refined estimate of tsunami source.
Result is an accurate forecast of tsunami.
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18. ADVANTAGE OF DART BUOYS
Seismometer do not measure tsunami.
Tidal gauge do not provide direct measurement of deep
ocean tsunami energy propagating.
DART overcomes drawback of both.
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19. WORKING OF DART BUOYS
DART BUOY consist of two main component:
• Bottom Pressure Recorder (BPR)
• Surface Buoy
BPR consisting of a modem to transmit data to surface
buoy.
Surface buoy transmit data to warning centre via satellite
communication.
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20. BOTTOM PRESSURE RECORDER:
Digiquartz Broadband depth Sensor is the main sensing
element.
This sensor continuously monitors pressure and if
pressure exceeds threshold value, it automatically report
to warning centre.
SURFACE BUOYS:
Surface buoys makes satellite communication to
warning centers that evaluate the threat and issue a
tsunami warning.
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22. DIGIQUARTZ BROADBAND DEPTH
SENSOR
This depth sensor provide accurate & stable data.
Superior performance of digiquartz instruments is
achieved through use of quartz crystal.
Pressure transducer employs bellows tube as pressure to
load generators.
Change in frequency of quartz crystal oscillator is a
measure of the applied pressure.
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23. ACOUSTIC TRANSDUCER
A electrical device that converts sound wave into
electrical energy.
Hydrophone is used in this case.
When electrical plates are exposed to sound vibration
electrical energy is produced.
Electrical energy is sent to amplifier and then to final
destination.
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24. ACOUSTIC LINK
Acoustic communication is a technique of sending and
receiving signals under water.
It is done by help of acoustic modem.
Modem operates at frequency of 10Hz – 1MHz.
It provides an accurate and efficient method to send and
receive data underwater.
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25. NOAA AND DART STATIONS
NOAA
(NATIONAL OCEANIC & ATMOSPHERIC ADMINISTRATION)
• Responsible for providing tsunami warning to the
nation.
DART
(DEEP OCEAN ASSESSMENT & REPORTING OF TSUNAMI)
• Station that detects tsunami.
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27. STANDARD MODE:
System generally operates in standard mode.
DART transmits data every six hours with recording
period of 15 minutes.
EVENT MODE:
When tsunami wave occur standard mode trigger to
event mode.
Transmit data every15 minutes at an average of 1 minute
for three hours.
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29. SERIES OF DART SYSTEM
There are two series of DART buoy system:
DART I
BUOY
DART II
BUOY
SERIES
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30. DART I SYSTEM
One way communication ability.
Relied solely on software’s ability to detect a tsunami
and trigger to event mode.
To avoid false alarm, a threshold value is set such that
tsunami with low amplitude could fail to trigger the
station.
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31. DART II SYSTEM
It is a two way communication
Measure seal level change of less than a millimeter in
the deep ocean.
Two way communication allows for trouble shooting of
the system.
System can be switched to event mode by concerned
authority for research purpose.
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32. ADVANTAGES
Deep water pressure produce low false reading.
Multiple sensor can detect wave propagation.
Good advance warning system.
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34. FUTURE SCOPE
Use of GPS to detect tsunami.
Developed by NASA.
GPS detects ground motion preceding tsunami.
It estimate tsunami destructive potential within minutes.
Estimates energy that undersea earthquake transfer to
ocean.
With help of these data, ocean floor displacement
caused by earthquake can be inferred.
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