Building Submarine Seismic Detection System Shang-Hsueh Yu a 、 Po-Chi Chen a 、 Jia-Pu Jang a 、 Chau-Chang Wang a,b,c 、 Ban-Yuan Kuo b a Taiwan Ocean Research.

Slides:



Advertisements
Similar presentations
SeaCycler AST2 Surface Piercing Profiler Technology.
Advertisements

Seismology Forum Meeting 2014:
Exploring Earthquakes By: Jordyn Friel and Kylie Edens.
Page created by W. G. Huang Mw= Mw= Mw= Mw= Mw= Mw= Mw=
Passive Aquatic Listener: A state-of-art system employed in Atmospheric, Oceanic and Biological Sciences in the Marine Environment Prof. E. N. Anagnostou,
Imaging the Deep Seismic Structure Beneath a Mid- Ocean Ridge: The MELT Experiment May 1998.
Instrumentation and Quantification of Tsunamis With an Emphasis on the Santa Barbara Channel.
Internal Tidal Currents in the Gaoping Submarine Canyon I-Huan Lee National Museum of Marine Biology and Aquarium,Pingtung, Taiwan, , R.O.C.
Tsunamis Detection The Mission  Tsunamis Detection can help to minimize loss of life and property from future tsunamis. Mission Introduction Mechanism.
How to prevent the interference of ship itself exhaust emissions when measurement air pollutants over the South China Sea during 2010 Yung-Yao Lan (1),
CENTER FOR COASTAL AND MARINE BIODIVERSITY, BHATYE-- RATNAGIRI.
SUPERSITES COORDINATION WORKSHOP Monday 10 June 2013
TWG Berne November 2005 EUREF High Rate GPS for Positioning, Atmospheric Effects and Natural Hazards Warning System EPN Study Group Chairmen G. Stangl.
Lecture #19- Seismometers
Preliminary Measurement of Submarine Groundwater Discharge in Taiwan Yi-Jie Lin*,Chen-Tung Arthur Chen, Meng-Chia Chen Institute of Marine Geology and.
What's Happening in the Bathtub?: An Overview of Present-Day Sea Level Change R. Steven Nerem University of Colorado Department of Aerospace Engineering.
Sri Lanka Earthquake & Tsunami Warning Training Program Session III.3 Global and Local Arrays May 10, 2006 Jakarta, Indonesia.
Real-time Monitoring of the Derwent and Huon Estuaries in Southern Tasmania Greg Timms Senior Research Scientist Tasmanian ICT Centre, CSIRO 20 May 2009.
Copyright © by Isiorho1 Earthquake Slides By Dr. S. A. Isiorho.
-for saving innocent lives
Earthquakes ● Earthquake: a sudden and violent shaking of Earth, caused by movements within the crust or volcanism ● Ex. San Francisco Earthquake in California.
Seismicity around Lhasa Tsoja Wangmo 1), Norsang Gelsor 1) and Jens Havskov 2) 1) Jiangsu Road No 36 Lhasa, Tibet, PRC 2) University of Bergen, Department.
NEPTUNE Transforming ocean science OCEAN NETWORKS CANADA EXPLORATION∙INNOVATION∙ACTION For a Changing Planet A University of Victoria Initiative Seismic.
Evidence on non-self-similarity source scaling in cluster earthquakes Yen-Yu Lin 1, Kuo -Fong Ma 1, Hiroo Kanamori 2, Teh-Ru Song 3, Nadia Lapusta 2, Victor.
Waves and Tsunamis Ralph Stephen, WHOI 29th Annual MME Conference April 30, 2005 Ralph Stephen, WHOI 29th Annual MME Conference April 30, 2005.
Tsunami Warning System Elements IOC Assessment Mission to Indonesia 29 August-1 September 2005.
Living (Rose Bengal Stained) Benthic Foraminifera in Sediments off the Southwest Taiwan Ai-Ping Chiang, Hui-Ling Lin, and Tai-Chun Lin Institute of Marine.
Introduction to the Broadband Array in Taiwan for Seismology (BATS) Wen-Tzong Liang* Chun-Chi Liu Bor-Shouh Huang Institute of Earth Sciences, Academia.
High Sensitivity Magnetic Gradiometer for Earthquake Research Applications ISRAEL 2005 Ivan Hrvoic H. Ginzburg, H. Zafrir, G. Steinitz, B. Shirman, G.
CALYPSO Seminar, 29 th of August of 2013 “Recent advances in the application of SeaSonde HF Radar technology to improve Operational Oceanography capacity”
New earthquake category Nature 447, (3 May 2007) | doi: /nature05780; Received 8 December 2006; Accepted 26 March A scaling law for slow.
IRIS workshop on “Managing Waveform Data and Related Metadata from Seismic Networks” Hotel Windsor Suites, Bangkok, Thailand 08-13, January, 2012 Ashvin.
Seismic Networks Operated by Central Weather Bureau in Taiwan Ta-Yi Chen Central Weather Bureau.
About National Sun Yat-sen Univ. The Logo of NSYSU.
Correlation Between Groundwater Level And Altitude Variations in Land Subsidence Area of The Choshuichi Alluvial Fan, Taiwan Chieh-Hung Chen, Chung-Ho.
Earthquakes Sudden movement of surface when accumulated strain along opposing sides of a fault is suddenly released. Rock stretches and snaps.
The existing and upgrading national seismological network in vietnam Le Tu Son Le Tu Son Institute of Geophysics, VAST Vietnam.
A Preliminary Report of Two Earthquakes Recorded by both Broadband and Rotation Sensors C. C. Liu 1, B. S. Huang 1, and W. H. K. Lee 2 1 Institute of Earth.
Fig 3) Crustal Structure using the tomography method, in the central part of Itoigawa- Shizuoka Tectonic Line (ISTL). The central part of the Itoigawa-Sizuoka.
Ocean Surface Current Observations in PWS Carter Ohlmann Institute for Computational Earth System Science, University of California, Santa Barbara, CA.
{ Ocean Topography topo= a place graphy= write. Why do we care? Why do we care?
Measuring Rotation Motions in the Free Field of Taiwan W. H. K. Lee U. S. Geological Survey, Menlo Park, CA 94025, USA C. C. Liu Institute of Earth Sciences,
Effects of Rotation Motions on a Seismogram Hung-Chie Chiu Institute of Earth Sciences, Academia Sinica, Taiwan March 19, 2014.
Seismograph Networks in Japan
Global and Local Arrays. Topics covered:  Types of seismic arrays  How arrays are used  Example global networks.
A Study on Characteristics of Seasonally Dependent Infrasound Propagation Based on the Ground-Truth Events from a Long- Term Experiment at a Quarry mine.
Tsunamis are caused by earthquakes, landslides, volcanic eruptions, or asteroid impacts. How tsunamis are caused.
Earthquake Information Page created by W. G. HuangCredit EMSC Summary: MagnitudeMw 7.2 RegionNEAR EAST COAST OF HONSHU, JAPAN Date time :45:17.0.
EARTHQUAKE REPORT SOUTH AMERICA WEEK OF JANUARY 27 TH TO FEBRUARY 2 ND, 2016 OLIVIA HELPRIN.
Development of Automatic Image Processing System for Sediment Tube Trap 1 C-C Wang, 2 S-Y Lin, 2 C-Y Chen, 3 J. Liu and 4 H.L. Lin 1 Institute of Applied.
BY K.MOUNIKA CSE 4 TH YEAR. What is a Tsunami? A tsunami is a wave in the ocean or in a lake that is created by a geologic event characterized by a series.
EARTHQUAKE REPORT SOUTH AMERICA WEEK OF FEBRUARY 3 RD TO FEBRUARY 9 TH, 2016 OLIVIA HELPRIN.
1 Ching-Hui Wu Department of Nuclear Regulation Atomic Energy Council, Taiwan September 23, 2013 An Overview of the Recommendations from NEA peer review.
Seismic phases and earthquake location
1 Center for Measurement Standards(CMS)-National Measurement Laboratory(NML) 2 Department of Civil Engineering,
NETWORK REPORT SRI LANKA Geological Survey & Mines Bureau Sri Lanka.
Profiling Float for Abyssal ocean Deep NINJA
South America EQ Report, Week 2
Strong Motion Network in Taiwan
Broadband Array in Taiwan for Seismology (BATS) Current Status
درون ماه چیست؟ به طور معمول از اندازه‌گیری‌های غیرمستقیم و مدل‌ها برای مطالعه‌ی ساختار و ترکیبات درون اجرام سیاره‌ای استفاده می‌شود ماه دارای هسته‌ای بسیار.
Earthquake report south America
Earthquakes Unit 12.2.
Teh-Quei Lee (1), Kuo-Yen Wei (2) and Chih-An Huh (1)
Tracking the Blue Whales Using ocean color satellite
Numerical Simulation of East China Sea Tsunami by Boussinesq Equation
Title Reporter: Your Name Advisor: Din Ping Tsai 21 April 2019
Earthquake Information
Effects of Rotation Motions on a Seismogram
70 Years of Seismology at DTM
Presentation transcript:

Building Submarine Seismic Detection System Shang-Hsueh Yu a 、 Po-Chi Chen a 、 Jia-Pu Jang a 、 Chau-Chang Wang a,b,c 、 Ban-Yuan Kuo b a Taiwan Ocean Research Institute, National Applied Research Laboratories, Kaohsiung, Taiwan b Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan c Institute of Applied Marine Physics and Undersea Technology, National Sun Yat-sen University, Kaohsiung, Taiwan Speaker : Yu Shang Hsueh

Motivation 2 Period : 2010/10/17 ~ 2011/10/17 ml ≧ 2 , Total : 9908 From CWB

3 YARDBIRD 1.LOG: 24 bit/4ch 、 sample rate: 100Hz 、 GPS time compensation 、 user interface. 2.Deployment period is 1 year, power dissipation must be less than 0.5W. 3.Currently maximum depth is 2000m 4.Leveling: Error is less than 1 ∘. Bandwidth: 4sec~40Hz. 5.Yardbird hangs flash beacon 、 radio beacon and flag for recovery. 6.Center of gravity and buoyancy for downward pose 、 rising and downward velocity. 7.Acoustic system for release and location Seismometer Buoy Acoustic system Camera Beacon Battery & Log Specifications

4 Seismometer 1. 3 perpendicular components 2. Leveling: Error is less than 1 ∘. 3.Bandwidth:4sec~40Hz.

5 Deployment Experiments

6 Recover

Local Seismic Data(1)

8 Local Seismic Data(2)

9 Teleseismic(1) 3.7 km/s3.5 km/s Qinghai earthquake, April 14, 2010 (21.917, ; depth is 1450 m)

10 MOU with KORDI in South Korea

11

12 Teleseismic(2) Magnitude 8.6 & OFF THE WEST COAST OF NORTHERN SUMATRA, April 11,2012 Yardbird deployed Korea’s East Sea Magnitude 8.6, 2.311°N, °E, 22.9 kmMagnitude 8.2, 0.773°N, °E, 16.4 km Raw data site

13 Future Works We completed 3 times long term(10 mouths) deployment and 4 times short term (2 weeks ~ 3 months) deployments successfully, and we will still continue research and development further, such as maximum depth will be extended to 6000m 、 channel numbers increase from 4 to 7 for more sensors 、 bandwidth extends from 4 s to 30 s. In order to fulfill the ultimate objective of building an engineering-, science-, and management-wise sustainable system in Taiwan, Our team will continue to work with more domestic universities and search international cooperation.

14 Thank You For Your Attention!! If more questions, please mail to our group! Mr. Chen, Po-Chi: Mr. Jang, Jia-Pu: Mr. Yu, Shang-Hsueh: