Atmospheric Pressure Change Associated with the 2003 Tokachi-Oki Earthquake Shingo Watada, Takashi Kunugi, Keinji Hiarata, Hiroko Sugioka, Kiwamu Nishida,

Slides:



Advertisements
Similar presentations
Patrick Smith Academic History PhD Project Title: Combining magma flow modelling and seismicity on Montserrat Supervisor: Prof. Jürgen Neuberg (aka Locko)
Advertisements

Development of an In-Situ Test for Direct Evaluation of the Liquefaction Resistance of Soils K. H. Stokoe, II, E. M. Rathje and B.R. Cox University of.
AN INERTIAL ROTATION METER (TILTMETER) Hutt, C. R., Holcomb, L. G., and Sandoval, L. D. USGS Albuquerque Seismological Laboratory Surface tilt noise has.
WAVE Characteristics March 24 – 27, 2015.
Seismic Wave Demonstrations and Animations L. Braile, Purdue University  Copyright L. Braile. Permission.
Seismic Wave Demonstrations and Animations L. Braile, Purdue University  Copyright L. Braile. Permission.
International Training Course, Potsdam ORFEUS Workshop, Vienna IRIS Metadata Workshop, Cairo 2009 IRIS Metadata Workshop, Foz do Iguacu 2010 E. Wielandt:
Making Waves: Seismic Waves Activities and Demonstrations Larry Braile, Purdue University web.ics.purdue.edu/~braile Sheryl Braile,
Seismic Wave Propagation
II.1 Theoretical Seismology 2: Wave Propagation
  The word comes from the Greek word seismic, for shaking.  It is the branch of Geology which has provided the most comprehensive interpretation of.
Lecture #19- Seismometers
Lecture-15 1 Lecture #15- Seismic Wave Overview. Lecture-15 2 Seismograms F Seismograms are records of Earth’s motion as a function of time.
Receivers and Recording Systems. Geophones String of Geophones 3 component Typical exploration geophone Various casings.
Wave Type (and names) Particle MotionOther Characteristics P, Compressional, Primary, Longitudinal Dilatational Alternating compressions (“pushes”) and.
UHM CanSat Team Members: Chris Ho: Team master, software Tyson Fukuyama: Hardware.
5: EARTHQUAKES WAVEFORM MODELING S&W SOMETIMES FIRST MOTIONS DON’T CONSTRAIN FOCAL MECHANISM Especially likely when - Few nearby stations, as.
PHYS 218 sec Review Chap. 15 Mechanical Waves.
Sri Lanka Earthquake & Tsunami Warning Training Program Session III.3 Global and Local Arrays May 10, 2006 Jakarta, Indonesia.
Focal Mechanism Solutions
-for saving innocent lives
Esci 411, Advanced Exploration Geophysics (Micro)seismicity John Townend EQC Fellow in Seismic Studies
How and where are earthquake waves detected and recorded? A seismograph is an instrument that records earthquake waves. It is also used to determine the.
Yuji Otake, Akito Araya and Kazuo Hidano
Vibrations from blasting
Geology 5660/6660 Applied Geophysics 17 Jan 2014 © A.R. Lowry 2014 Read for Wed 22 Jan: Burger (Ch 2.2–2.6) Last time: The Wave Equation; The Seismometer.
Sri Lanka Earthquake & Tsunami Warning Training Program Session III.3 Global and Local Arrays April 5, 2006 CETRAC, Sri Lanka.
Project IDA (International Deployment of Accelerometers) Project IDA Station Installation Issues and Techniques IRIS Metadata Workshop August 13, 2010.
・ Rays Snell ’ s Law Structure of the Earth ・ Seismic Waves Near-Field Terms (Static Displacements) Far-Field Terms (P, S, Surface waves) ・ Normal modes.
Earthquake – A sudden release of stored energy. This energy has built up over long periods of time as a result of tectonic forces within the earth.
Portable Broadband Seismic Stations - Checking Data Quality Cairo, Egypt November, 2009 Noel Barstow Bruce Beaudoin Marcos Alvarez.
IntroductionModern Seismology – Data processing and inversion 1 Modern Seismology Lecture Outline Seismic networks and data centres Mathematical background.
Seismological Perspectives on Broadband Tilt, Strain, and Rotation Measurement Charles Langston Center for Earthquake Research and Information University.
Properties of Waves. Mechanical Waves Mechanical wave requires a medium – such as rope, air, water or soil The wave begins at a source, this causes molecules.
THE ANALYSIS OF THE INFRASOUND SIGNALS FROM MAY 12 EARTHQUAKE WENCHUAN CHINA Wang Xiaohang Signal Processing Department North China Institute of Computing.
Waves: An introduction
Theoretical Seismology 2: Wave Propagation
An Assessment of the High-Gain Streckheisen STS2 Seismometer for Routine Earthquake Monitoring in the US ISSUE: Is the high-gain STS2 too sensitive to.
Capturing the “hum” of the Earth on low frequency seismic arrays Barbara Romanowicz Univ of California, Berkeley in collaboration with: Junkee Rhie.
Waves. Simple Harmonic Motion  periodic motion - a motion that ________itself again and again along the same path  simple harmonic motion (SHM) - a.
HIGH FREQUENCY GROUND MOTION SCALING IN THE YUNNAN REGION W. Winston Chan, Multimax, Inc., Largo, MD W. Winston Chan, Multimax, Inc., Largo, MD Robert.
Industrial Noise and Vibration Solution for Session 2 Physical Acoustics
P wave amplitudes in 3D Earth Guust Nolet, Caryl Michaelson, Ileana Tibuleac, Ivan Koulakov, Princeton University.
Graphing Trig Functions Review Whiteboard Activity.
ITW2007 Infra-red image of a typhoon (by JMA) Mt. Anatahan eruption ( ) photo by Patrick Shore Total eclipse Photo by Katsuya Ishikawa.
Waves. What are waves? A wave is a transfer of energy from one place to another. Waves take many forms. Wave Characteristics include: –Amplitude –Wavelength.
Geology 5660/6660 Applied Geophysics 20 Jan 2016
As you can see, low frequencies are not absorbed as well. This means low frequencies will travel farther. That graph comes from this extremely detailed.
Gaetano Festa, Aldo Zollo, Simona Colombelli, Matteo Picozzi, Alessandro Caruso Dipartimento di Fisica; Università di Napoli Federico II.
September 18, 2002Ahmed Elgamal 1 Seismic Waves Ahmed Elgamal.
Monitoring of the tidal variations in the seismic and hydrogeological data collected at the East European Platform Besedina A.N., Kabychenko N.V., Gorbunova.
EaRtHqUaKeS!. More than 700 Earthquakes that are strong enough to cause damage occur every year. Earthquakes are caused by stress applied to rocks from.
1 SITE RESPONSE ANALYSIS USING MICROTREMORS Boğaziçi University Kandilli observatory and Earthquake Research Institute Department of Geophysics Korhan.
Good Morning! Have out on your desk, “How do Waves Transfer Energy?” In your notebook, answer the following questions: 1. Name two ways you can apply force.
Fermilab 21cm Morocco Site Evaluation Status Kermit Carlson John Marriner Dave McGinnis Ralph Pasquinelli December 22, 2008.
Cabled systems for near-field tsunami early warning: An observation system simulation experiment (OSSE) offshore Portugal A. Babeyko1, M. Nosov2 and.
WAVE Characteristics.
Lecture 11 WAVE.
Sheryl Braile, Happy Hollow School West Lafayette, IN
Uplift: Faults and Earthquakes
Waves Check your notes!.
Seismic Wave Propagation
MEE …. WAVE PROPAGATION IN SOLIDS
 Earthquake Zones • About 95 percent of the major earthquakes occur in a few narrow zones.
Seismic Wave Propagation
REF TEK Technology Overview
Making Waves: Seismic Waves Activities and Demonstrations
ورود اطلاعات بصورت غيربرخط
Waves.
Presentation transcript:

Atmospheric Pressure Change Associated with the 2003 Tokachi-Oki Earthquake Shingo Watada, Takashi Kunugi, Keinji Hiarata, Hiroko Sugioka, Kiwamu Nishida, Shoji Sekiguchi, Jun Oikawa, Yoshinobu Tsuji, Hiroo Kanamori

microbarogram2003/09/26 24 hour 1000sec JIZODO STS1 vault

Software configuration Microbarograph recording and telemetry systems Hardware configuration GPS antenna Sensor Control PC

On-line board PC based system SGN (Yamanashi, Japan) Air battery Portable sensor Board PC Microbarograph sensor Off-line recording system

Ground vertical velocity Filtered atmospheric pressure 3.2km/sec atmosphere Ground

atmosphere Ground for homogeneous fluid

Observational transfer function

Mechanical sensitivty check by shake table

Theoretical transfer function of long-period atmospheric waves. atmosphere Ground for homogeneous fluid High frequency asymptote for propagating acoustic waves

Conclustion The atmospheric pressure change associted with the 2003 Tokachi-Oki earthquake are observed at the co-located site of broadband seismometers. The origin of atmospheric pressure change is the Rayleigh waves passing at the site. The observational transfer functions, both phase and amplitude, are constructed and compared with the theoretical transfer functions and found consistent up to 50 sec.