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ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola Campus, Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO) IMS, Installation and Certification Group, Acoustic Monitoring Project e-mail: [email protected] ITW2007: P. Campus Tokyo, 13-16 November 2007

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Page 1: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

The IMS Infrasound Network: detection of a large variety of events, including volcanic

eruptionsDr. Paola Campus,

Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO) IMS, Installation and Certification Group, Acoustic Monitoring Project

e-mail: [email protected]

ITW2007: P. Campus Tokyo, 13-16 November 2007

Page 2: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Examples of infrasound signals

Page 3: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

The International Monitoring

System (IMS) Infrasound Network

Page 4: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Earthquakes

Irian Jaya, 2002/10/10, Mw=7.5IS07, Warramunga, NT, Australia:

~2000km

Page 5: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Irian Jaya, 2002/10/10, Mw=7.5IS07

Page 6: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Irian Jaya, 2002/10/10, Mw=7.5IS07

Page 7: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Irian Jaya, 2002/10/10, Mw=7.5IS07: seismic waves

Page 8: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Irian Jaya, 2002/10/10, Mw=7.5IS07: seismic waves

Page 9: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Irian Jaya, 2002/10/10, Mw=7.5IS07: infrasound waves

Page 10: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Irian Jaya, 2002/10/10, Mw=7.5IS07: infrasound waves

Page 11: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Infrasound might help complement the information about earthquakes especially

when, for local events, local seismic networks are very sparse or non existing

Earthquakes

Page 12: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Bolides

Chicago fireball, 2003/03/27

Page 13: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

A few minutes after midnight (local time) on March 27, 2003, a huge bolide entered

the atmosphere, moving across Ohio, Illinois, Indiana and Wisconsin and

producing a luminous blue flash.

Fragments of the bolide hit an inhabited area of about 10 km, located south of

Chicago.

Chicago fireball

Page 14: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Chicago fireball, IS10, Lac du Bonnet, Canada: ~1170km

Page 15: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Chicago fireball, IS10, Lac du Bonnet, Canada: ~1170km

Page 16: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Chicago fireball, IS10, Lac du Bonnet, Canada: ~1170km

Page 17: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Two different bolides following two different trajectories?

Chicago fireball, IS10, Lac du Bonnet, Canada: ~1170km

Page 18: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Chicago fireball, IS10, Lac du Bonnet, Canada: ~1170km

Page 19: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Chicago fireball, IS10, Lac du Bonnet, Canada: ~1170km

Page 20: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Movements of glaciers and calving of icebergs

IS18, Qaanaaq, Northern Greenland, Danemark

Page 21: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18, Qaanaaq, Northern Greenland

Page 22: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18, Qaanaaq, Northern Greenland

Page 23: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18, infrasound signals: freq. 0.4-6 Hz

Page 24: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18: long duration infrasound signal freq. 0.4-6 Hz

Page 25: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Slow movement of glacier or tide associated to it?

IS18: long duration infrasound signal freq. 0.4-6 Hz

Page 26: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18: short duration infrasound signal 1: freq. 0.4-6 Hz

Page 27: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18: short duration infrasound signal 1: freq. 0.4-6 Hz

Page 28: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18: short duration infrasound signal 2: freq. 0.4-6 Hz

Page 29: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18: short duration infrasound signal 2: freq. 0.4-6 Hz

Page 30: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18: short duration infrasound signal 3: freq. 0.4-6 Hz

Page 31: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS18: short duration infrasound signal 3: freq. 0.4-6 Hz

Page 32: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Infrasound might help monitor the effects of global warming through the systematic observation of movements of glaciers and

calving of icebergs

Movements of glaciers and calving of icebergs

Page 33: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Volcanoes

Page 34: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Volcanic hazard: a serious threat to

-Nearby settlements-Civil Aviation

The IMS Infrasound Network can contribute to volcano monitoring

Page 35: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

The increased number of IMS Infrasound Stations allows us to monitor several active volcanic

areas around the world

Page 36: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Aleutian Islands

Page 37: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

AUGUSTINE Alaska, Aleutian Islands,

Kamishak Bay, Southern Cook Inlet 59.363N, 153.43W; summit elev. 1,252 m

Augustine is the most active volcano of the eastern Aleutian arc.

On January 13, 2006 the volcano entered a period of repetitive and explosive eruptions. Each event produced

ash plumes, mudflows, and pyroclastic flows

Volcanoes

Page 38: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

AUGUSTINE, 59.363N, 153.43W, 1252m

Page 39: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

AUGUSTINE, 59.363N, 153.43W, 1252m

Page 40: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS53: Dist. ~ 675 km; Prop.Time ~00:37

Frequency band: 0.4-8 Hz

Page 41: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS53: Dist. ~ 675 km; Prop.Time ~00:37

Frequency band: 0.4-8 Hz

Page 42: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

Kamchatka Peninsula

Page 43: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

KARYMSKY Kamtchatka Peninsula, Russian Federation 54.05°N, 159.43°E; summit elev. 1,536 m

Karymsky is the most active volcano of the eastern volcanic zone of Kamtchatka.

Growth of the lava dome since the end of 2005. Several ash explosions on the beginning of 2006.

First example: ash plumes registered on 2006/01/12. No origin time was available

Volcanoes

Page 44: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

KARYMSKY, 54.0N, 159.5E, 4875m

Page 45: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS44, Petropavlovsk-Kamchatski, Russian Federation

Page 46: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS44: Dist.~154km; Prop.Time ~00:08

Frequency band: 0.4-6 Hz

Page 47: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS44: Dist.~154km; Prop.Time ~00:08

Frequency band: 0.4-6 Hz

Page 48: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS44: Dist.~154km; Prop.Time ~00:08

Frequency band: 0.4-6 Hz

Page 49: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

KARYMSKY

Two events close in time, with no significant variation in the meteorological conditions

(wind speed, wind direction, temperature):

the difference in the waveforms can be associated to differences in the source

Volcanoes

Page 50: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

KARYMSKY

From 07 May to 14 May the seismicity was above background levels, with 330-450 shallow

earthquakes per day. Based on seismic data, possible ash and gas explosions.

No origin time was available

Volcanoes

Page 51: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS44: Dist.~154km; Prop.Time ~00:08

Frequency band: 0.4-8 Hz

Page 52: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

IS44: Dist.~154km; Prop.Time ~00:08

Frequency band: 0.4-8 Hz

Page 53: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

The presence of an infrasound station in a volcanic area can be extremely useful to

monitor the beginning of an eruption and to define its origin time. In addition, an

infrasound station can be used both as a unique volcano monitoring tool in case other

monitoring systems are not available (or cannot be used), and as a complementary tool to other, already existing, monitoring systems.

Page 54: ITW2007: P. Campus Tokyo, 13-16 November 2007 The IMS Infrasound Network: detection of a large variety of events, including volcanic eruptions Dr. Paola

ITW2007: P. Campus Tokyo, 13-16 November 2007

The IMS Infrasound Network is not only a powerful tool to monitor nuclear explosions, but it can also provide a significant contribution to monitor natural events:•Complement or provide information about earthquakes •Complement or provide information about bolides, meteorites, auroras•Monitor effects of global warming•Complement or provide information about volcanic eruptions (origin time, source characteristics)

Conclusions