A Multi-Purpose Continuous GPS Network within the boundary zones of the Eurasian, African, and Arabian plates

Size: px
Start display at page:

Download "A Multi-Purpose Continuous GPS Network within the boundary zones of the Eurasian, African, and Arabian plates"

Transcription

1 A Multi-Purpose Continuous GPS Network within the boundary zones of the Eurasian, African, and Arabian plates Bahadır AKTUĞ General Command of Mapping TR06100 Ankara/Turkey

2 Anatolia, as a natural laboratory for geosciences: Transform strike-slip faulting Continental collision Major thrust faulting Continental escape Subduction Contraction Extension

3

4 GPS STUDIES İN TURKEY date back to early 1990s geodynamics-oriented at the earlier stage focused on seismically i active areas high concentration in Marmara and Western Anatolia >80 GPS survey campaigns since 1992

5 TURKISH NATIONAL FUNDAMENTAL GPS NETWORK TURKISH NATIONAL FUNDAMENTAL GPS NETWORK (TNFGN)

6 TURKISH NATIONAL FUNDAMENTAL GPS NETWORK (TNFGN) Established between 1997 and 1999 ~600 stations a spatial resolution of km Periodic measurements between 1999 and o o 40 o 39 o 38 o 37 o 36 o o o o o o o o o o o

7 TURKISH NATIONAL PERMANENT GPS NETWORK (TNPGN)

8 ~25 stations Concentrated mostly in Western Anatolia Functional > 5 years 4 of them are included in IGS and EPN Still geodynamics-orientedoriented No real-time

9 Ankara (ANKR) Istanbul (ISTA) Trabzon (TRAB) Gebze (TUBI) IGS IGS/EPN Stations in Turkey Tracking Networks EPN

10 A new Multi-purpose Real-time Network: TURKISH NATIONAL PERMANENT GPS RTK NETWORK for Surveying/Cadastre Geodynamics/Earthquake Hazard Assessment Meteorology (Troposphere) Communications (Ionosphere) Long-term Earthquake prediction Short-term term Earthquake-prediction? (ionosphere?)

11 A Multi-Purpose Continuous GPS Network in Turkey TURKISH NATIONAL PERMANENT GPS RTK NETWORK Distribution of TNPGN TNPGN and T TNPGN NPGN--Active stations (as of Jun 2008). Red Circles TPGN sitessites-27; Blue Triangles: TPGN TPGN--ACTIVE stations(145).

12 TURKISH NATIONAL PERMANENT GPS RTK NETWORK Homogenously distributed ib t d across Anatolia Fully functional by the end of 2008 Communications on ADSL/GPRS VRS-FKP-MAC support Static mode for geodynamics/reference frame issues Kinematic prospects with 20 Hz update rate( Deformation monitoring etc.)

13 TPGN Konya Station (a) (b) (c) TPGN-ACTIVE pillar types (a) ground (b) terrace (c) roof

14 Turkish National Fundamental GPS Network (TNFGN) 80 GPS survey campaigns since 1992 Turkish National Fundamental GPS Network (TNFGN) in 1999 A spatial resolution of km Periodic measurements between 1999 and 2007 Turkish National Permanent GPS Network (TNPGN) ~25 stations Functional > 5 years 4 of them are IGS Static data Turkish National GPS RTK Network (TNGRN) 145 stations Fully-functional by the end of 2008 A spatial resolution of ~75 km Real-time and static data.

15 GPS METEOROLOGY More than half of the GPS stations installed in meteorological parks of General Directorate of State Meteorology. Precipitable it water (PW) data: Radio-sounding Application in Turkey: Spatial Resolution : 7 stations Temporal Resolution : ½ day GPS-Derived PW Application in Turkey: Spatial Resolution : 145 stations Temporal Resolution : 30 sec at near real-time with unprecedented temporal and spatial coverage.

16 GPS METEOROLOGY Preliminary tests at selected stations. High-quality surface meteorological data for GPS stations. 40 Radiosonde GPS ANKR STATION

17 Good agreement at PW values between radiosonde and GPS Rms (0.2 mm) well below average uncertainties (0.5 mm) Histogram of Differences Between GPS And Radiosonde Derived PWs At ANKR Station in mm

18 Surface vs. Mean Atmospheric Temperature ISTANBUL (COAST) ANKR (LAND) Weigh ted mean atmosph heric temperature (K) Surface temperature (K) Surface temperature (K)

19 Current Issues: Topografic relief in Turkey up to 5 km (Western Anatolia at near sea-level and mountainous Eastern Anatolia) Different Empirical coefficients (?) needed to relate Surface temperature to Mean Atmospheric Temp. Not easy assimilation of GPS-derived precipitable water data with numerical weather models. Near real-time data processing (kinematic or moving window?) ISTANBUL (COAST) ANKR (LAND) d mean atmospheric temperature (K) Weighted Surface temperature (K) Surface temperature (K)

20 REAL-TIME IONOSPHERIC TOMOGRAPHY Project initiated between GCM and Hacettepe University Real-time 3D mapping of ionosphere Supported by Turkish Scientific and Technological Research Council (TUBITAK)

21 REAL-TIME IONOSPHERIC TOMOGRAPHY Independent software implementation Currently code observations only Estimation of receiver DCBs at non-igs stations

22 Much denser velocity field need even for low-accuracy works Much lower correlation in vertical velocities Velocity Field in ITRF00-NNR

23 Broader deformation zone Plate-assignment of sites is almost impossible near NAFZ and EAFZ Velocity Field in a Eurasia-Fixed Frame

24 Systematic increase of velocites towards West Non-rigid Central Anatolia? Velocity Field in an Anatolia-Fixed Frame

25 Rigid-body rotation expected to be ~1-2 0 /Myr Non-uniform deformation? Rigid-body Rotations in 0 /Myr

26 Delineates the main fault zones Shows active strike-slip fault zones in Cental Anatolia Shear strains in nanostrain/yr

27 In Summary; New Turkish National GPS RTK Network (TNGRN) will provide a spatial resolution of ~75 km with 145 stations real-time cm-level positioning for survey community invaluable data for weather forecasting real-time TEC data for ionospheric mapping a network for studying earthquake hazard assesment in a very active geography insights about the unresolved issues within the boundary zones of Eurasian, African, and Arabian plates

28 THANK YOU!

Recent GNSS Developments and Reference Frame Issues in Turkey. Onur LENK and Bahadir AKTUĞ

Recent GNSS Developments and Reference Frame Issues in Turkey. Onur LENK and Bahadir AKTUĞ Recent GNSS Developments and Reference Frame Issues in Turkey Onur LENK and Bahadir AKTUĞ General Command of Mapping onur.lenk lenk@hgk.mil.tr 1/31 GPS STUDIES İN TURKEY date back to early 1990s geodynamics-oriented

More information

Slip Rates Estimate of Western North Anatolian Fault System in Turkey

Slip Rates Estimate of Western North Anatolian Fault System in Turkey Slip Rates Estimate of Western North Anatolian Fault System in Turkey Haluk OZENER, Asli DOGRU, Bahadir AKTUG, Semih ERGINTAV, Bulent TURGUT, Onur YILMAZ, Kerem HALICIOGLU, Onur GURKAN, Turkey Keywords:

More information

GPS study of N-S trending Karaburun Belt (Turkey) and its E-W trending eastern part

GPS study of N-S trending Karaburun Belt (Turkey) and its E-W trending eastern part Presented at the FIG Working Week 2017, GPS study of N-S trending Karaburun Belt (Turkey) and its E-W trending eastern part May 29 - June 2, 2017 in Helsinki, Finland Muzaffer KAHVECİ Selcuk University,

More information

Determination of Current Velocity Field (Rate) of North Anatolian Fault in Izmit-Sapanca Segment

Determination of Current Velocity Field (Rate) of North Anatolian Fault in Izmit-Sapanca Segment Determination of Current Velocity Field (Rate) of North Anatolian Fault in Izmit-Sapanca Segment Cetin MEKIK, Bulent TURGUT, Haluk OZENER, Turkish Republic INTRODUCTION Turkey is geologically the part

More information

An Analysis of Strain Accumulation in the Western Part of Black Sea Region in Turkey

An Analysis of Strain Accumulation in the Western Part of Black Sea Region in Turkey An Analysis of Strain Accumulation in the Western Part of Black Sea Region in Turkey Ilke DENIZ, Nevin Betul AVSAR, Rasim DENIZ, Cetin MEKIK, Senol Hakan KUTOGLU, Turkey Key words: Deformation measurement,

More information

INSAR ATMOSPHERIC DELAY MIGITIGATION BY GPS; CASE STUDY IZMIT EARTQUAKE INTERFEROGRAMS

INSAR ATMOSPHERIC DELAY MIGITIGATION BY GPS; CASE STUDY IZMIT EARTQUAKE INTERFEROGRAMS INSAR ATMOSPHERIC DELAY MIGITIGATION BY GPS; CASE STUDY IZMIT EARTQUAKE INTERFEROGRAMS M.U. Altın a, *, E. Tari a, L. Ge b a ITU, Civil Engineering Faculty, 80626 Maslak Istanbul, Turkey (altinm, tari)@itu.edu.tr

More information

GNSS METEOROLOGY AND WATER VAPOUR ESTIMATION IN TURKEY

GNSS METEOROLOGY AND WATER VAPOUR ESTIMATION IN TURKEY GNSS METEOROLOGY AND WATER VAPOUR ESTIMATION IN TURKEY DR. CETIN MEKIK ASSOC. PROF., THE DEPT. OF GEOMATICS ENGINEERING BULENT ECEVIT UNIVERSITY, ZONGULDAK/TURKEY GNSS4SWEC MC&WG Meeting, Varna, Bulgaria,

More information

Tectonic deformations in Greece and the operation of HEPOS network

Tectonic deformations in Greece and the operation of HEPOS network Tectonic deformations in Greece and the operation of HEPOS network M. Gianniou KTIMATOLOGIO S.A. (Hellenic Cadastre) Abstract Today, networks of permanent reference stations are broadly used for the realization

More information

NATIONAL SEISMIC NETWORKS OF TURKEY

NATIONAL SEISMIC NETWORKS OF TURKEY Ministry of Public Works and Settlement General Directorate of Disaster Affairs EARTHQUAKE RESEARCH DEPARMENT (GDDA- ERD) NATIONAL SEISMIC NETWORKS OF TURKEY RELEMR WORKSHOP İSTANBUL - 2008 Sami ZÜNBÜL

More information

GEODETIC NETWORK OF SAUDI ARABIA AND FIDUCIAL STATIONS. GFN OF Saudi Arabia in Based on ITRF2000 Datum

GEODETIC NETWORK OF SAUDI ARABIA AND FIDUCIAL STATIONS. GFN OF Saudi Arabia in Based on ITRF2000 Datum STUDIES OF TECTONIC MOVEMENTS IN SAUDI ARABIA USING CORS M. Al Rajhi, Ali Al Omar, R. Yanar, F. Kartal, K. Eren, SUBJECT TO TALKS BACKGROUND GEODETIC NETWORK OF SAUDI ARABIA AND FIDUCIAL STATIONS GFN OF

More information

Determination of Velocity Field and Strain Accumulation of Densification Network in Marmara Region

Determination of Velocity Field and Strain Accumulation of Densification Network in Marmara Region Determination of Velocity Field and Strain Accumulation of Densification Network in Marmara Region M.Sc.Ilke DENIZ Assoc.Prof.Dr. Haluk OZENER Istanbul Technical University I.T.U. Ayazaga Kampusu, Insaat

More information

How GNSS CORS in Japan works for geodetic control and disaster mitigations

How GNSS CORS in Japan works for geodetic control and disaster mitigations ICG Working Group D Reference Frames, Timing and Applications How GNSS CORS in Japan works for geodetic control and disaster mitigations ICG11, Nov. 7-11, 2016, Sochi, Russia Hiromichi TSUJI Geodetic Observation

More information

The problem (1/2) GPS velocity fields in plate boundary zones are very smooth. What does this smoothness hide?

The problem (1/2) GPS velocity fields in plate boundary zones are very smooth. What does this smoothness hide? Block models The problem (1/2) GPS velocity fields in plate boundary zones are very smooth Figure from Tom Herring, MIT What does this smoothness hide? Continuous deformation? Rigid block motions, with

More information

ESTIMATES OF HORIZONTAL DISPLACEMENTS ASSOCIATED WITH THE 1999 TAIWAN EARTHQUAKE

ESTIMATES OF HORIZONTAL DISPLACEMENTS ASSOCIATED WITH THE 1999 TAIWAN EARTHQUAKE ESTIMATES OF HORIZONTAL DISPLACEMENTS ASSOCIATED WITH THE 1999 TAIWAN EARTHQUAKE C. C. Chang Department of Surveying and Mapping Engineering Chung Cheng Institute of Technology, Taiwan, ROC ABSTRACT A

More information

Dealing with significant differential tectonic plate velocities within an RTK-network: The case of HEPOS

Dealing with significant differential tectonic plate velocities within an RTK-network: The case of HEPOS Dealing with significant differential tectonic plate velocities within an RTK-network: The case of HEPOS M. Gianniou, E. Mitropoulou, I. Stavropoulou National Cadastre and Mapping Agency S.A. Mesogion

More information

CONTENTS 1. INTRODUCTION (STUDY AREA) 3. PROCESSING (CONVENTIAL& GPS) 4. ANALYSIS OF OUTCOMES 5. CONCLUSIONS 2. THE GCM-ITU NETWORK SURVEYING

CONTENTS 1. INTRODUCTION (STUDY AREA) 3. PROCESSING (CONVENTIAL& GPS) 4. ANALYSIS OF OUTCOMES 5. CONCLUSIONS 2. THE GCM-ITU NETWORK SURVEYING INVESTIGATION OF THE DISPLACEMENTS FROM 1941 TO 2007 USING TERRESTRIAL AND GPS MEASUREMENTS ALONG THE WESTERN PART OF NORTH ANATOLIAN FAULT IN MARMARA REGION G. Akay 1 and H. Ozener 2,1 [1]{Bogazici University,

More information

SUPPLEMENTARY INFORMATION

SUPPLEMENTARY INFORMATION SUPPLEMENTARY INFORMATION doi: 10.1038/ngeo739 Supplementary Information to variability and distributed deformation in the Marmara Sea fault system Tobias Hergert 1 and Oliver Heidbach 1,* 1 Geophysical

More information

NTUA, Faculty of Rural and Surveying Engineering, Dionysos Satellite Observatory, Higher Geodesy Laboratory NOA, Institute of Geodynamics 1

NTUA, Faculty of Rural and Surveying Engineering, Dionysos Satellite Observatory, Higher Geodesy Laboratory NOA, Institute of Geodynamics 1 NOA, Institute of Geodynamics 1 Crustal Deformation from GPS measurements at the Ionian Sea : Preliminary Results Anastasiou 1 D., Paradissis 1 D., Ganas 2 A., Marinou 1 A., Papazissi 1 K., Drakatos 2

More information

An Analysis of Strain Accumulation in the Western Part of Black Sea Region in Turkey

An Analysis of Strain Accumulation in the Western Part of Black Sea Region in Turkey An Analysis of Strain Accumulation in the Western Part of Black Sea Region in Turkey Ilke DENIZ, Nevin Betul AVSAR, Rasim DENIZ, Cetin MEKIK, Senol Hakan KUTOGLU ideniz@beun.edu.tr, nb_avsar@beun.edu.tr,

More information

ANALYSIS OF SPATIAL AND TEMPORAL VARIATION OF EARTHQUAKE HAZARD PARAMETERS FROM A BAYESIAN APPROACH IN AND AROUND THE MARMARA SEA

ANALYSIS OF SPATIAL AND TEMPORAL VARIATION OF EARTHQUAKE HAZARD PARAMETERS FROM A BAYESIAN APPROACH IN AND AROUND THE MARMARA SEA ANALYSIS OF SPATIAL AND TEMPORAL VARIATION OF EARTHQUAKE HAZARD PARAMETERS FROM A BAYESIAN APPROACH IN AND AROUND THE MARMARA SEA Y. Bayrak 1, T. Türker 2, E. Bayrak 3 ABSTRACT: 1 Prof Dr. Geophysical

More information

Earth s Tectonic Plates

Earth s Tectonic Plates MASTER 49 6.2 3.7 5.4 Philippine Pacific 5.4 North American Juan de Fuca Caribbean Cocos 10.0 9.2 2.3 2.5 2.3 1.8 3.0 Indian-Australian 10.5 7.1 17.2 16.8 6.0 Nazca South American 11.1 10.3 7.3 3.7 7.5

More information

Gözde AKAY and Haluk OZENER, Turkey

Gözde AKAY and Haluk OZENER, Turkey Investigation of the Displacements from 1941 to 2007 using Terrestrial and Gps Measurements along the Western Part of North Anatolian Fault in Marmara Region Gözde AKAY and Haluk OZENER, Turkey Key words:

More information

Realizing a geodetic reference frame using GNSS in the presence of crustal deformations: The case of Greece

Realizing a geodetic reference frame using GNSS in the presence of crustal deformations: The case of Greece Realizing a geodetic reference frame using GNSS in the presence of crustal deformations: The case of Greece M. Gianniou National Cadastre and Mapping Agency S.A. Outline 1. Introduction 2. Deformation

More information

Diagram 1. Diagram What kind of crust is plate A, B and C made of? 2. What type of plate boundary is shown at X?

Diagram 1. Diagram What kind of crust is plate A, B and C made of? 2. What type of plate boundary is shown at X? Diagram 1 1. What kind of crust is plate A, B and C made of? 2. What type of plate boundary is shown at X? 3. What plate boundary is shown at Y? 4. What is being shown at Z? Why is plate B going underneath

More information

The Earthquake of Padang, Sumatra of 30 September 2009 scientific information and update

The Earthquake of Padang, Sumatra of 30 September 2009 scientific information and update The Earthquake of Padang, Sumatra of 30 September 2009 scientific information and update 01-October-2009 Christophe Vigny Directeur de recherches at CNRS Laboratoire de Géologie Geoscience Dept. Of ENS,

More information

Using Cascais GPS Permanent Station for geodynamic purposes.

Using Cascais GPS Permanent Station for geodynamic purposes. Using Cascais GPS Permanent Station for geodynamic purposes. Ribeiro, H. 1 e Pinto, J.T. 1 1 IPCC Instituto Português de Cartografia e Cadastro, Portugal SUMMARY Cascais GPS station, the first Portuguese

More information

NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2

NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2 NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2 Assignment is due the beginning of the class period on December 14, 2004. Mark answers on a scantron sheet, which will be provided.

More information

CONTINENTAL PLATE BOUNDARY ZONES

CONTINENTAL PLATE BOUNDARY ZONES CONTINENTAL PLATE BOUNDARY ZONES Plate boundaries initially viewed as narrow Now recognize that many plate boundaries - especially continental - are deformation zones up to 1000 km wide, with motion spread

More information

Operational Aspects of GNSS CORS What is a GNSS CORS system used for?

Operational Aspects of GNSS CORS What is a GNSS CORS system used for? Please insert a picture (Insert, Picture, from file). Size according to grey field (10 cm x 25.4 cm). Scale picture: highlight, pull corner point Cut picture: highlight, choose the cutting icon from the

More information

NCC roles in successful disaster response I.R.IRAN

NCC roles in successful disaster response I.R.IRAN The Second UN-GGIM-AP Plenary Meeting NCC roles in successful disaster response I.R.IRAN Teheran Iran 28-30 October 2013 Ali Javidaneh Technical Deputy of National Cartographic Center (NCC) Outline Types

More information

We have processed RO data for climate research and for validation of weather data since 1995 as illustrated in Figure 1.

We have processed RO data for climate research and for validation of weather data since 1995 as illustrated in Figure 1. Real-time Analysis of COSMIC Data Christian Rocken, Doug Hunt, Bill Schreiner University Corporation for Atmospheric Research (UCAR) COSMIC Project Office Boulder, CO Abstract UCAR has analyzed GPS radio

More information

The PaTrop Experiment

The PaTrop Experiment Improved estimation of the tropospheric delay component in GNSS and InSAR measurements in the Western Corinth Gulf (Greece), by the use of a highresolution meteorological model: The PaTrop Experiment N.

More information

GEO-VIII November Geohazard Supersites and Natural Laboratories Progress Report. Document 9

GEO-VIII November Geohazard Supersites and Natural Laboratories Progress Report. Document 9 GEO-VIII 16-17 November 2011 Geohazard Supersites and Natural Laboratories Progress Report Document 9 This document is submitted to GEO-VIII for information. Geohazard Supersites and Natural Laboratories

More information

Activity Pacific Northwest Tectonic Block Model

Activity Pacific Northwest Tectonic Block Model Activity Pacific Northwest Tectonic Block Model The Cascadia tectonic margin is caught between several tectonic forces, during the relentless motions of the giant Pacific Plate, the smaller subducting

More information

Lateral extrusion and tectonic escape in Ilan Plain of northeastern Taiwan

Lateral extrusion and tectonic escape in Ilan Plain of northeastern Taiwan Lateral extrusion and tectonic escape in Ilan Plain of northeastern Taiwan Angelier, J., Chang, T.Y., Hu, J.C., Chang, C.P., Siame, L., Lee, J.C., Deffontaines, B., Chu, H.T, Lu, C.Y., Does extrusion occur

More information

GPS Strain & Earthquakes Unit 5: 2014 South Napa earthquake GPS strain analysis student exercise

GPS Strain & Earthquakes Unit 5: 2014 South Napa earthquake GPS strain analysis student exercise GPS Strain & Earthquakes Unit 5: 2014 South Napa earthquake GPS strain analysis student exercise Strain Analysis Introduction Name: The earthquake cycle can be viewed as a process of slow strain accumulation

More information

Report for 15th PCGIAP Meeting at 18th UNRCC-AP Working Group 1 Regional Geodesy

Report for 15th PCGIAP Meeting at 18th UNRCC-AP Working Group 1 Regional Geodesy Report for 15th PCGIAP Meeting at 18th UNRCC-AP Working Group 1 Regional Geodesy Chairman Shigeru Matsuzaka, Japan - shigeru@gsi.go.jp Vice Chairman Prof. Pengfei Cheng, China - chengpf@casm.ac.cn John

More information

GG S. Internal Vision of GGOS. Markus Rothacher. GFZ Potsdam

GG S. Internal Vision of GGOS. Markus Rothacher. GFZ Potsdam Internal Vision of GGOS Markus Rothacher GFZ Potsdam GGOS Retreat DGFI in Munich February 15-16, 2006 Contents Motivation Four Levels of Products of the IAG Services: First Level: Raw Data Collection Second

More information

Geodetic Department KTIMATOLOGIO S.A. (Hellenic Cadastre) K. Katsampalos, C. Kotsakis Department of Geodesy and Surveying

Geodetic Department KTIMATOLOGIO S.A. (Hellenic Cadastre) K. Katsampalos, C. Kotsakis Department of Geodesy and Surveying Realization of ETRS89 in Greece by the HEPOS network M. Gianniou i Geodetic Department KTIMATOLOGIO S.A. (Hellenic Cadastre) mgianniu@ktimatologio.gr K. Katsampalos, C. Kotsakis Department of Geodesy and

More information

Empirical Green s Function Analysis of the Wells, Nevada, Earthquake Source

Empirical Green s Function Analysis of the Wells, Nevada, Earthquake Source Nevada Bureau of Mines and Geology Special Publication 36 Empirical Green s Function Analysis of the Wells, Nevada, Earthquake Source by Mendoza, C. 1 and Hartzell S. 2 1 Centro de Geociencias, Universidad

More information

Scattering and intrinsic attenuation structure in Central Anatolia, Turkey using BRTR (PS-43) array

Scattering and intrinsic attenuation structure in Central Anatolia, Turkey using BRTR (PS-43) array Scattering and intrinsic attenuation structure in Central Anatolia, Turkey using BRTR (PS-43) array CTBT: Science & Technology 2011 Korhan Umut SEMIN Nurcan Meral OZEL B.U. Kandilli Observatory & Earthquake

More information

Chapter Review USING KEY TERMS. asthenosphere uplift continental drift. known as. tectonic plates move. object. UNDERSTANDING KEY IDEAS

Chapter Review USING KEY TERMS. asthenosphere uplift continental drift. known as. tectonic plates move. object. UNDERSTANDING KEY IDEAS Skills Worksheet Chapter Review USING KEY TERMS 1. Use the following terms in the same sentence: crust, mantle, and core. Complete each of the following sentences by choosing the correct term from the

More information

IMPACT OF GROUND-BASED GPS PRECIPITABLE WATER VAPOR AND COSMIC GPS REFRACTIVITY PROFILE ON HURRICANE DEAN FORECAST. (a) (b) (c)

IMPACT OF GROUND-BASED GPS PRECIPITABLE WATER VAPOR AND COSMIC GPS REFRACTIVITY PROFILE ON HURRICANE DEAN FORECAST. (a) (b) (c) 9B.3 IMPACT OF GROUND-BASED GPS PRECIPITABLE WATER VAPOR AND COSMIC GPS REFRACTIVITY PROFILE ON HURRICANE DEAN FORECAST Tetsuya Iwabuchi *, J. J. Braun, and T. Van Hove UCAR, Boulder, Colorado 1. INTRODUCTION

More information

The Global Geodetic Observing System (GGOS) of the International Association of Geodesy, IAG

The Global Geodetic Observing System (GGOS) of the International Association of Geodesy, IAG The Global Geodetic Observing System (GGOS) of the International Association of Geodesy, IAG Hans-Peter Plag (1), Markus Rothacher (2), Richard Gross (3), Srinivas Bettadpur (4) (1) Nevada Bureau of Mines

More information

Seven years of postseismic deformation following the 1999, M = 7.4 and M = 7.2, Izmit-Düzce, Turkey earthquake sequence

Seven years of postseismic deformation following the 1999, M = 7.4 and M = 7.2, Izmit-Düzce, Turkey earthquake sequence JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114,, doi:10.1029/2008jb006021, 2009 Seven years of postseismic deformation following the 1999, M = 7.4 and M = 7.2, Izmit-Düzce, Turkey earthquake sequence S. Ergintav,

More information

Seismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake

Seismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake J-RAPID Symposium March 6-7, 2013 Seismic Activity and Crustal Deformation after the 2011 Off the Pacific Coast of Tohoku Earthquake Y. Honkura Tokyo Institute of Technology Japan Science and Technology

More information

Algerian Space Agency Center of Space Techniques

Algerian Space Agency Center of Space Techniques Algerian Space Agency Center of Space Techniques Investigation of deformations in North of Algeria with GPS data and kinematic model Radia MIR, Salem ahlouche, Saïd Touam Space Geodesy Division Center

More information

ON NEAR-FIELD GROUND MOTIONS OF NORMAL AND REVERSE FAULTS FROM VIEWPOINT OF DYNAMIC RUPTURE MODEL

ON NEAR-FIELD GROUND MOTIONS OF NORMAL AND REVERSE FAULTS FROM VIEWPOINT OF DYNAMIC RUPTURE MODEL 1 Best Practices in Physics-based Fault Rupture Models for Seismic Hazard Assessment of Nuclear ON NEAR-FIELD GROUND MOTIONS OF NORMAL AND REVERSE FAULTS FROM VIEWPOINT OF DYNAMIC RUPTURE MODEL Hideo AOCHI

More information

The continental lithosphere

The continental lithosphere Simplicity to complexity: The continental lithosphere Reading: Fowler p350-377 Sampling techniques Seismic refraction Bulk crustal properties, thickness velocity profiles Seismic reflection To image specific

More information

ON THE RELATION BETWEEN GPS STRAIN FIELD AND ACTIVE FAULTS IN THE EASTERN BALTIC REGION

ON THE RELATION BETWEEN GPS STRAIN FIELD AND ACTIVE FAULTS IN THE EASTERN BALTIC REGION ON THE RELATION BETWEEN GPS STRAIN FIELD AND ACTIVE FAULTS IN THE EASTERN BALTIC REGION B.A. Assinovskaya 1, V.L. Gorshkov 2, N.V. Shcherbakova 2, N.M. Panas 1 1 Geophysical Service RAS, seismic station

More information

A new transformation including deformation model for the Nordic. and Baltic countries

A new transformation including deformation model for the Nordic. and Baltic countries A new transformation including deformation model for the Nordic Presented at the FIG Working Week 2017, May 29 - June 2, 2017 in Helsinki, Finland and Baltic countries P. Häkli, M. Lidberg, L. Jivall,

More information

GEORED Project: GNSS Geodesy Network for Geodynamics Research in Colombia, South America. Héctor Mora-Páez

GEORED Project: GNSS Geodesy Network for Geodynamics Research in Colombia, South America. Héctor Mora-Páez GEORED Project: GNSS Geodesy Network for Geodynamics Research in Colombia, South America. Héctor Mora-Páez Colombian Geological Survey UNAVCO SCIENCE MEETING Feb 27 March 1, 2012 Boulder, CO, TECTONIC

More information

3. PLATE TECTONICS LAST NAME (ALL IN CAPS): FIRST NAME: PLATES

3. PLATE TECTONICS LAST NAME (ALL IN CAPS): FIRST NAME: PLATES LAST NAME (ALL IN CAPS): FIRST NAME: PLATES 3. PLATE TECTONICS The outer layers of the Earth are divided into the lithosphere and asthenosphere. The division is based on differences in mechanical properties

More information

IS THE SUDETIC MARGINAL FAULT STILL ACTIVE? RESULTS OF THE GPS MONITORING

IS THE SUDETIC MARGINAL FAULT STILL ACTIVE? RESULTS OF THE GPS MONITORING Acta Geodyn. Geomater.Vol.1, No.3 (135), 35-39, 2004 IS THE SUDETIC MARGINAL FAULT STILL ACTIVE? RESULTS OF THE GPS MONITORING 1996-2002 Bernard KONTNY Department of Geodesy and Photogrammetry, Agricultural

More information

Geometry of co-seismic surface ruptures and tectonic meaning of the 23 October 2011 Mw 7.1 Van earthquake (East Anatolian Region, Turkey)

Geometry of co-seismic surface ruptures and tectonic meaning of the 23 October 2011 Mw 7.1 Van earthquake (East Anatolian Region, Turkey) Geometry of co-seismic surface ruptures and tectonic meaning of the 23 October 2011 Mw 7.1 Van earthquake (East Anatolian Region, Turkey) Bülent Dogan & Ahmet Karakaș. Journal of Structural Geology, 46(2013),

More information

Deformation of Rocks. Orientation of Deformed Rocks

Deformation of Rocks. Orientation of Deformed Rocks Deformation of Rocks Folds and faults are geologic structures caused by deformation. Structural geology is the study of the deformation of rocks and its effects. Fig. 7.1 Orientation of Deformed Rocks

More information

1. occurs when the oceanic crust slides under the continental crust.

1. occurs when the oceanic crust slides under the continental crust. 1. occurs when the oceanic crust slides under the continental crust. 2. What type of stress is shown? 3. Where two plates slide past one another is called a boundary. 4. What type of stress is shown? 5.

More information

SOURCE MODELING OF RECENT LARGE INLAND CRUSTAL EARTHQUAKES IN JAPAN AND SOURCE CHARACTERIZATION FOR STRONG MOTION PREDICTION

SOURCE MODELING OF RECENT LARGE INLAND CRUSTAL EARTHQUAKES IN JAPAN AND SOURCE CHARACTERIZATION FOR STRONG MOTION PREDICTION SOURCE MODELING OF RECENT LARGE INLAND CRUSTAL EARTHQUAKES IN JAPAN AND SOURCE CHARACTERIZATION FOR STRONG MOTION PREDICTION Kimiyuki Asano 1 and Tomotaka Iwata 2 1 Assistant Professor, Disaster Prevention

More information

Development of a Predictive Simulation System for Crustal Activities in and around Japan - II

Development of a Predictive Simulation System for Crustal Activities in and around Japan - II Development of a Predictive Simulation System for Crustal Activities in and around Japan - II Project Representative Mitsuhiro Matsu'ura Graduate School of Science, The University of Tokyo Authors Mitsuhiro

More information

Spatio-temporal variation in slip rate on the plate boundary off Sanriku, northeastern Japan, estimated from small repeating earthquakes

Spatio-temporal variation in slip rate on the plate boundary off Sanriku, northeastern Japan, estimated from small repeating earthquakes Spatio-temporal variation in slip rate on the plate boundary off Sanriku, northeastern Japan, estimated from small repeating earthquakes T. Matsuzawa, N. Uchida, T. Igarashi *, N. Umino, and A. Hasegawa

More information

Sn attenuation in the Anatolian and Iranian plateau and surrounding regions

Sn attenuation in the Anatolian and Iranian plateau and surrounding regions Published as: Gok, R., Sandvol, E., Turkelli, N., Seber, D., and Barazangi, M., 2003. Sn attenuation in the Anatolian and Iranian plateau and surrounding regions, Geophys. Res. Lett., 30(24). Sn attenuation

More information

Tectonics. Planets, Moons & Rings 9/11/13 movements of the planet s crust

Tectonics. Planets, Moons & Rings 9/11/13 movements of the planet s crust Tectonics Planets, Moons & Rings 9/11/13 movements of the planet s crust Planetary History Planets formed HOT Denser materials fall to center Planet cools by conduction, convection, radiation to space

More information

USU 1360 TECTONICS / PROCESSES

USU 1360 TECTONICS / PROCESSES USU 1360 TECTONICS / PROCESSES Observe the world map and each enlargement Pacific Northwest Tibet South America Japan 03.00.a1 South Atlantic Arabian Peninsula Observe features near the Pacific Northwest

More information

Deformation of the Crust

Deformation of the Crust Deformation of the Crust Review Choose the best response. Write the letter of that choice in the space provided. 1. The state of balance between the thickness of the crust and the depth at which it rides

More information

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn Plate Tectonics By Destiny, Jarrek, Kaidence, and Autumn .The Denali Fault and San Andreas Fault - The San Andreas Fault is a continental transform fault that extends roughly 1300 km (810 miles) through

More information

The Mw 6.2 Leonidio, southern Greece earthquake of January 6, 2008: Preliminary identification of the fault plane.

The Mw 6.2 Leonidio, southern Greece earthquake of January 6, 2008: Preliminary identification of the fault plane. The Mw 6.2 Leonidio, southern Greece earthquake of January 6, 28: Preliminary identification of the fault plane. J. Zahradnik 1, E. Sokos 2, A.Serpetsidaki 2, and G A.Tselentis 2 1 Charles University in

More information

9th Workshop on Three-Dimensional Modelling of Seismic Waves Generation, Propagation and their Inversion

9th Workshop on Three-Dimensional Modelling of Seismic Waves Generation, Propagation and their Inversion 1965-36 9th Workshop on Three-Dimensional Modelling of Seismic Waves Generation, Propagation and their Inversion 22 September - 4 October, 2008 Tomography and Active Tectonics in Kanto, Japan Francis T.

More information

GPS Strain & Earthquakes Unit 3: Finding location and velocity data for PBO GPS stations

GPS Strain & Earthquakes Unit 3: Finding location and velocity data for PBO GPS stations GPS Strain & Earthquakes Unit 3: Finding location and velocity data for PBO GPS stations Original activity by Vince Cronin (Baylor University). Revisions by Beth Pratt-Sitaula (UNAVCO). Analyzing the velocities

More information

Geotechnical Earthquake Engineering Prof. Deepankar Choudhury Department of Civil Engineering Indian Institute of Technology, Bombay

Geotechnical Earthquake Engineering Prof. Deepankar Choudhury Department of Civil Engineering Indian Institute of Technology, Bombay Geotechnical Earthquake Engineering Prof. Deepankar Choudhury Department of Civil Engineering Indian Institute of Technology, Bombay Module - 3 Lecture - 7 Engineering Seismology (Contd ) Let us start

More information

Monitoring and Analyzing Movements of Geodetic Monuments

Monitoring and Analyzing Movements of Geodetic Monuments Serdar EROL, Bihter EROL and Rahmi Nurhan ÇELİK, Turkey Key words: IGS, GPS, Inclination Sensor, Spectral Analysis, Wavelet Analysis SUMMARY The movements of a pillar in 1.20 m height, which is an IGS

More information

5. INTEGRATED EXAMPLES FROM REAL EQs.

5. INTEGRATED EXAMPLES FROM REAL EQs. 5. INTEGRATED EXAMPLES FROM REAL EQs. Some strong seismic events occurred in the Greek territory, during the period 2003-2007 of the operation of the installed, monitoring network, for the registration

More information

TECTONIC MOVEMENTS MONITORING OF SUDETIC MARGINAL FAULT USING SHORT GPS BASELINES

TECTONIC MOVEMENTS MONITORING OF SUDETIC MARGINAL FAULT USING SHORT GPS BASELINES POSTER PAPER SESSION TECTONIC MOVEMENTS MONITORING OF SUDETIC MARGINAL FAULT USING SHORT GPS ASELINES ernard Kontny Department of Geodesy and Photogrammetry Agricultural University of Wroclaw, Poland Abstract

More information

Case Study of Japan: Crustal deformation monitoring with GNSS and InSAR

Case Study of Japan: Crustal deformation monitoring with GNSS and InSAR Technical Seminar Reference Frame in Practice, Case Study of Japan: Crustal deformation monitoring with GNSS and InSAR Basara Miyahara miyahara-b96ip@milt.go.jp Geospatial Information Authority of Japan

More information

Active deformation in eastern Indonesia and the Philippines from GPS and seismicity data

Active deformation in eastern Indonesia and the Philippines from GPS and seismicity data JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 105, NO. B1, PAGES 663-680, JANUARY 10, 2000 Active deformation in eastern Indonesia and the Philippines from GPS and seismicity data Corn6 Kreemer and William E.

More information

Principles of the Global Positioning System Lecture 24

Principles of the Global Positioning System Lecture 24 12.540 Principles of the Global Positioning System Lecture 24 Prof. Thomas Herring http://geoweb.mit.edu/~tah/12.540 OVERVIEW Examination of results from Earthscope Reference frame definition: SNARF High-rate

More information

CHAPTER 1 BASIC SEISMOLOGY AND EARTHQUAKE TERMINOLGY. Earth Formation Plate Tectonics Sources of Earthquakes...

CHAPTER 1 BASIC SEISMOLOGY AND EARTHQUAKE TERMINOLGY. Earth Formation Plate Tectonics Sources of Earthquakes... CHAPTER 1 BASIC SEISMOLOGY AND EARTHQUAKE TERMINOLGY Earth Formation... 1-2 Plate Tectonics... 1-2 Sources of Earthquakes... 1-3 Earth Faults... 1-4 Fault Creep... 1-5 California Faults... 1-6 Earthquake

More information

STUDY ON APPROPRIATE MODELING OF TSUNAMIS IN MALAYSIA FOR RISK EVALUATION

STUDY ON APPROPRIATE MODELING OF TSUNAMIS IN MALAYSIA FOR RISK EVALUATION STUDY ON APPROPRIATE MODELING OF TSUNAMIS IN MALAYSIA FOR RISK EVALUATION Zaty Aktar binti Mokhtar* Supervisor: Fumihiko Imamura** MEE06025 Shunichi Koshimura** ABSTRACT In order to design a tsunami warning

More information

Introduction to Displacement Modeling

Introduction to Displacement Modeling Introduction to Displacement Modeling Introduction Deformation on the Earth surface informs us about processes and material properties below surface Observation tools: GPS (static-dynamic) InSAR (static)

More information

Continuous monitoring of seismicity by Indian permanent seismological observatory at Maitri

Continuous monitoring of seismicity by Indian permanent seismological observatory at Maitri Indian Journal of Marine Sciences Vol. 37(4), December 2008, pp. 396-403 Continuous monitoring of seismicity by Indian permanent seismological observatory at Maitri E.C Malaimani*, N. Ravi Kumar, Simanchal

More information

Plate Tectonics Comic Book Pg s 9-13

Plate Tectonics Comic Book Pg s 9-13 Plate Tectonics Comic Book Pg s 9-13 Your Comic Book should include the following on each page: Your CHARACTER thoroughly explaining the concept for the page DRAWINGS for each of the topics A brief EXPLANATION

More information

Actual Continuous Kinematic Model (ACKIM) of the Earth s Crust based on ITRF2014

Actual Continuous Kinematic Model (ACKIM) of the Earth s Crust based on ITRF2014 Actual Continuous Kinematic Model (ACKIM) of the Earth s Crust based on ITRF2014 Hermann Drewes Technische Universität München Joint Scientific Assembly of the International Association of Geodesy and

More information

Supplementary Material

Supplementary Material 1 Supplementary Material 2 3 4 Interseismic, megathrust earthquakes and seismic swarms along the Chilean subduction zone (38-18 S) 5 6 7 8 9 11 12 13 14 1 GPS data set We combined in a single data set

More information

Establishment Of Gnss Regional Network For Tropospheric Tomography

Establishment Of Gnss Regional Network For Tropospheric Tomography Establishment Of Gnss Regional Network For Tropospheric Tomography Emine TANIR KAYIKÇI, Yasemin ŞIŞMAN, Selma ZENGIN KAZANCI, Cansu BEŞEL, Seldanur ÇELIK, Mesut DEMIRCAN, Turkey Key words: Severe weather,

More information

Africa-Arabia-Eurasia plate interactions and implications for the dynamics of Mediterranean subduction and Red Sea rifting

Africa-Arabia-Eurasia plate interactions and implications for the dynamics of Mediterranean subduction and Red Sea rifting This page added by the GeoPRISMS office. Africa-Arabia-Eurasia plate interactions and implications for the dynamics of Mediterranean subduction and Red Sea rifting Authors: R. Reilinger, B. Hager, L. Royden,

More information

On the Development and Implementations of the New Semi- Dynamic Datum for Indonesia

On the Development and Implementations of the New Semi- Dynamic Datum for Indonesia On the Development and Implementations of the New Semi- Dynamic Datum for Indonesia SusiloSUSILO 1, HasanuddinZ. ABIDIN 2, IrwanMEILANO 2, Benyamin SAPEII 2 1) Center for Geodetic Control Network and Geodynamic,

More information

Seven years of postseismic deformation following the 1999, M = 7.4 and M = 7.2, Izmit-Düzce, Turkey earthquake sequence

Seven years of postseismic deformation following the 1999, M = 7.4 and M = 7.2, Izmit-Düzce, Turkey earthquake sequence Seven years of postseismic deformation following the 1999, M = 7.4 and M = 7.2, Izmit-Düzce, Turkey earthquake sequence The MIT Faculty has made this article openly available. Please share how this access

More information

Regional deformation and kinematics from GPS data

Regional deformation and kinematics from GPS data Regional deformation and kinematics from GPS data Jessica Murray, Jerry Svarc, Elizabeth Hearn, and Wayne Thatcher U. S. Geological Survey Acknowledgements: Rob McCaffrey, Portland State University UCERF3

More information

Interdisciplinary Framework to Reveal Earthquake Precursory Phenomena in Seismically Active Areas

Interdisciplinary Framework to Reveal Earthquake Precursory Phenomena in Seismically Active Areas Interdisciplinary Framework to Reveal Earthquake Precursory Phenomena in Seismically Active Areas D.Ouzounov 1,2, S.Pulinets 3, M.Kafatos 1, P.Taylor 2 1 Chapman University, Orange, CA 92866, USA 2 NASA

More information

Earth s Interior StudyGuide

Earth s Interior StudyGuide Name Date Period Earth s Interior StudyGuide 1. The two main elements that make up the Earth s crust are and. 2. The Earth s inner core is made of solid and. 3. When one plates slides under another plate

More information

Important information from Chapter 1

Important information from Chapter 1 Important information from Chapter 1 Distinguish between: Natural hazard // Disaster // Catastrophe What role does human population play in these categories? Know how to read a Hazard Map, such as Figure

More information

Lab 9: Satellite Geodesy (35 points)

Lab 9: Satellite Geodesy (35 points) Lab 9: Satellite Geodesy (35 points) Here you will work with GPS Time Series data to explore plate motion and deformation in California. This lab modifies an exercise found here: http://www.unavco.org:8080/cws/pbonucleus/draftresources/sanandreas/

More information

Magnitude 7.1 NEAR THE EAST COAST OF HONSHU, JAPAN

Magnitude 7.1 NEAR THE EAST COAST OF HONSHU, JAPAN Japan was rattled by a strong aftershock and tsunami warning Thursday night nearly a month after a devastating earthquake and tsunami flattened the northeastern coast. This earthquake can be considered

More information

Dynamic Crust Practice

Dynamic Crust Practice 1. Base your answer to the following question on the cross section below and on your knowledge of Earth science. The cross section represents the distance and age of ocean-floor bedrock found on both sides

More information

THE ASSIMILATION OF SURFACE-SENSITIVE MICROWAVE SOUNDER RADIANCES AT ECMWF

THE ASSIMILATION OF SURFACE-SENSITIVE MICROWAVE SOUNDER RADIANCES AT ECMWF THE ASSIMILATION OF SURFACE-SENSITIVE MICROWAVE SOUNDER RADIANCES AT ECMWF Enza Di Tomaso and Niels Bormann European Centre for Medium-range Weather Forecasts Shinfield Park, Reading, RG2 9AX, United Kingdom

More information

CORS Network and Datum Harmonisation in the Asia-Pacific Region. Richard Stanaway and Craig Roberts

CORS Network and Datum Harmonisation in the Asia-Pacific Region. Richard Stanaway and Craig Roberts CORS Network and Datum Harmonisation in the Asia-Pacific Region Richard Stanaway and Craig Roberts School of Surveying and Spatial Information Systems University of New South Wales CORS Networks in the

More information

MAR110 Lecture #5 Plate Tectonics-Earthquakes

MAR110 Lecture #5 Plate Tectonics-Earthquakes 1 MAR110 Lecture #5 Plate Tectonics-Earthquakes Figure 5.0 Plate Formation & Subduction Destruction The formation of the ocean crust from magma that is upwelled into a pair of spreading centers. Pairs

More information

SOCIAL STUDIES GENERAL

SOCIAL STUDIES GENERAL GEOGRAPHY, MILITARY Maps War - Greece and Turkey War - Greece and Turkey 1920-1922 (p1) 1920-1922 (p2) Dieppe (p1) Dieppe (p2) Dieppe (p3) Dieppe (p4) Dieppe (p5) 120 GEOGRAPHY, MILITARY Maps Allied advances

More information

FORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.

FORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. FORCES ON EARTH UNIT 3.2 An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. USE THESE NOTES: OUR HOME PLANET EARTH: What do you know about our planet? SO.HOW

More information

P32 Temporal and Spatial Variations of b-value in the Western Anatolia

P32 Temporal and Spatial Variations of b-value in the Western Anatolia P32 Temporal and Spatial Variations of b-value in the Western Anatolia E. Bayrak* (Karadeniz Technical University) & Y. Bayrak (Karadeniz Technical University) SUMMARY The b-value calculated in time and

More information

Low-Latency Earthquake Displacement Fields for Tsunami Early Warning and Rapid Response Support

Low-Latency Earthquake Displacement Fields for Tsunami Early Warning and Rapid Response Support Low-Latency Earthquake Displacement Fields for Tsunami Early Warning and Rapid Response Support Hans-Peter Plag, Geoffrey Blewitt Nevada Bureau of Mines and Geology and Seismological Laboratory University

More information