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

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

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

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

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

This presentation covers the following areas

SIRGAS: Basis for Geosciences, Geodata, and Navigation in Latin America

Lab 9: Satellite Geodesy (35 points)

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

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

ESTIMATES OF HORIZONTAL DISPLACEMENTS ASSOCIATED WITH THE 1999 TAIWAN EARTHQUAKE

FORMAT FOR TECHNICAL PAPERS

Next Generation Australian Datum. Permanent Committee on Geodesy, ICSM

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

Case study of Japan: Reference Frames in Practice

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

The Impact of the 2010 Darfield (Canterbury) Earthquake on the Geodetic Infrastructure in New Zealand 1

What are the social, technical, environmental and economic benefits and opportunities of accessing and sharing geodetic data?

Geodesy on the move. Craig Allinson. Dealing with dynamic coordinate reference systems. IOGP Geodesy Subcommittee. EPUG London, November 2017

A Unique Reference Frame: Basis of the Global Geodetic Observing System (GGOS) for Geodynamics and Global Change

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

Using Cascais GPS Permanent Station for geodynamic purposes.

NATRF 2022 AND LDP OCTOBER 11, 2017

Do we need to update PNG94 to PNG2020?

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

Frames for the Future New Datum Definitions for Modernization of the U.S. National Spatial Reference System

Geodesy. orientation. shape. gravity field

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

Semi-Dynamic Datum of Indonesia

A Deformation Model to support a Next Generation Australian Geodetic Datum

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

Rigid Plate Transformations to Support PPP and Absolute Positioning in Africa

GGSP: Realisation of the Galileo Terrestrial Reference Frame

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

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

Publ. Astron. Obs. Belgrade No. 91 (2012), REALIZATION OF ETRF2000 AS A NEW TERRESTRIAL REFERENCE FRAME IN REPUBLIC OF SERBIA

DETERMINATION OF THE STATION COORDINATES FOR QUALITY CONTROL OF THE SATELLITE LASER RANGING DATA S.

The National Spatial Reference System of the Future

Positioning in the Pacific Islands

System of Geodetic Parameters Parametry Zemli 1990 PZ-90.11

Case Study of Australia

NGS and the Modernization of the National Spatial Reference System (NSRS)

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

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

The Victorian Seismic Zone 2011 GNSS Campaign Data Analysis

BUILDING AN ACCURATE GIS

Tectonic deformations in Greece and the operation of HEPOS network

Making Sense of Evolving Reference Frames for North America

International boundaries on a dynamic planet issues relating to plate tectonics and reference frame changes

Military Geographic Institute

The development and implementation of New Zealand Geodetic Datum 2000

The International Terrestrial Reference System and ETRS89: Part I : General concepts

CHILEAN PART OF SIRGAS REFERENCE FRAME, REALIZATION, ADOPTION, MAINTENANCE AND ACTUAL STATUS. Geodesy for Planet Earth IAG 2009, Buenos Aires

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

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

TOWARDS ROBUST LOCALIZATION OF RTK-GPS TOPOGRAPHIC SURVEYS 23

Update on the International Terrestrial Reference Frame (ITRF) : ITRF2014. Zuheir Altamimi

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

Reference frames and positioning

NCC roles in successful disaster response I.R.IRAN

FIG Asia Pacific Capacity Development Network

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

EUREF Technical Note 1: Relationship and Transformation between the International and the European Terrestrial Reference Systems

The PaTrop Experiment

Activity - Using GPS Data and Geologic Markers to Track Plate Motion

GPS measurements of current crustal movements along the Gulf of Suez, Egypt.

On the Use of Crustal Deformation Models. in the Management of ETRS89 Realizations in Fennoscandia

Estimation of tectonic velocities using GPS Precise Point Positioning: The case of Hellenic RTK network HEPOS

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

MODERNIZATION OF THE NSRS

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

Earthquakes and Faulting

Modernization of National Geodetic Datum in China *

GPS Surveying Dr. Jayanta Kumar Ghosh Department of Civil Engineering Indian Institute of Technology, Roorkee. Lecture 06 GPS Position

EXPLORE PLATE TECTONICS & MORE THROUGH GPS DATA. Shelley Olds, UNAVCO April 12, 2018 NGSS Webinar

Week 02. Assist. Prof. Dr. Himmet KARAMAN

MSGIC Spring Mtg Denton April 23, 2014

Weather Satellite Data Applications for Monitoring and Warning Hazard at BMKG

Combining InSAR, Levelling and GNSS for the Estimation of 3D Surface Displacements

Preparation for the ITRF2013. Zuheir Altamimi Xavier Collilieux Laurent Métivier IGN, France

A National Geocentric Datum and the Administration of Marine Spaces in Malaysia 2

Athanassios Ganas,

National Report of Greece to EUREF 2016

Positioning the Pacific: NOAA s Geospatial Activities. Juliana Blackwell, Director NOAA s National Geodetic Survey March 6, 2012

Evidence for plate tectonics

Gözde AKAY and Haluk OZENER, Turkey

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

Deformation monitoring and analysis using Victorian regional CORS data

Working Group 1. Geodetic Reference Frame. Activity Report. for. The UN-GGIM-AP Plenary Meeting

An Assessment of the Accuracy of PPP in Remote Areas in Oman

I. INTRODUCTION II. EARTHQUAKES

NGS is Scheduled to Replace NAVD 88 and NAD 83 In 2022

THREE SEASONAL BEHAVIOUR OF THE BALKAN PENINSULA GNSS PERMANENT STATIONS FROM GPS SOLUTIONS

A new era of geodetic big data - challenges and opportunities Tim Wright (COMET, University of

DETERMINATION OF GEOID IN THE KINGDOM OF SAUDI ARABIA USING GLOBAL GRAVITY MODEL AND GPS/BENCHMARK DATA: A CASE STUDY.

The U.S. National Spatial Reference System in 2022

Country Report On Sdi Activities In Singapore ( )

Volcanoes Session. Chairs: Y. Fukushima & G. Puglisi

The role of CORS GNSS data for climate monitoring: case study using NIGNET network

Analysis of Positional Displacement in Bohol Island on Aftermath of the 2013 Central Visayas Earthquake from GNSS Surveys

Country Report on SDI Activities in Singapore *

Transcription:

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 Saudi Arabia in 2004.0 Based on ITRF2000 Datum GFN OF Saudi Arabia in 2012.7 Based on ITRF2008 Datum TECTONIC DISPLACEMENTS FROM 2004 TO 2012 CONCLUDING REMARKS

BACKGROUND Scientific contribution of national CORS National CORS effectively serve the scientific studies related to atmosphere and ionospheric phenomena. Another scientific contribution of national CORS is the precise determination of displacements due to earthquakes, plate tectonics, volcanic eruptions, landslides etc. BACKGROUND TheEarthismadeofmanyplates.

BACKGROUND The Arabian plate moves towards the Eurasian plate, squeezing Anatolian plate Earthquakes have been the great natural hazard that threatens the Middle East region socially and economically. Tectonic setting of Turkey together with Arabian Plate (from Reilinger et al., 2006) Hence, it is crucial to have knowledge on the characteristics and dynamics of the tectonic fault lines to mitigate this hazard BACKGROUND Earthquake prone countries, like Turkey, need to take precautionary measures in advance to mitigate the consequences of natural hazards. During recent decades, the studies aimed at learning the plate mechanisms accelerated after the introduction of space-based application tools such as GNSS and radar image acquisition systems. CORS-TR data from 141 stations recorded during January 1st 2009 and November 30th 2009 were processed using the GAMIT/GLOBK program. The maximum displacement estimated ranged 19.9 mm/year toward southwest and 23.2 mm/year toward northwest. Plate displacements from 11 months CORS-TR surveys in 2009 XXV International Federation of Surveyors Congress, Kuala

GEODETIC NETWORK OF SAUDI ARABIA AND FIDUCIAL STATIONS GFN OF Saudi Arabia in 2004.0 Based on ITRF2000 Datum GFN OF Saudi Arabia in 2012.7 Based on ITRF2008 Datum A project was started in 2004 in order to establish a new geodetic network based on ITRF2000 datum (Epoch: 2004.0), known as MTRF2000. It consists of two parts: Geodetic Fiducial Network (GFN: 13 stations) Geodetic Main Network (GMN: 659 stations) GFN OF Saudi Arabia in 2004.0 Based on ITRF2000 Datum The GFN consisted of 13 highly accurate Fiducial stations across Saudi Arabia, each with a permanently tracking icgrs Ashtech Global Positioning System (GPS) receiver. The coordinates of all GFN stations were determined together with eight IGS stations using 10 days observations. The statistics of GFN GPS Surveys and Computations are: 8 x IGS stations were used as fixed reference stations 10 days data in 2004 (DOY 96-101, i.e. 5 10 April 2004) collected in 13 GFN sites, ITRF-2000 datum used, Processed the data for 1997.0 and 2004.0 epochs using the Geo++ GPS software XXV International Federation of Network adjustment was carried out and mm-level accuracy Surveyors was obtained Congress, Kuala for each GFN station (i.e. about 0.01 ppm precision results).

MTRF-2000 DEFINITION Datum MGD-2000 Reference Frame ITRF-2000 (International Terrestrial Reference Frame 2000), Epoch:2004.0 Ellipsoid Semi-major axis (a) Inverse flattening (1/f) Grid coordinates (Universal Transverse Mercator) GRS80 6,378,137.0 meters 298.257222101 Map Grid of MGD-2000 XXV International Federation of Surveyors Congress, Kuala GFN OF Saudi Arabia in.3 Based on ITRF2008 Datum Due to recent developments in technology, icgrs Ashtech Global Positioning System (GPS) receivers replaced with Leica GR25 GNSS receivers capable of measuring, GPS, GLONASS and Galileo signals, during January July 2012. The new coordinates of all GFN stations were determined together with eight IGS stations using 11 days observations. The statistics of GFN GPS Surveys and Computations are: 8 x IGS stations were used as fixed reference stations, 11 days data in (DOY 14-24, i.e. 14-24 January ) collected in 12 GFN sites, ITRF-2008 datum used, Processed the data for.3 epoch using BERNESE software packages Network adjustment was carried out and mm-level accuracy was XXV obtained International for Federation each GFNof station (i.e. about 0.01 ppm precision results). Surveyors Congress, Kuala

TECTONIC DISPLACEMENTS FROM 2004 TO The precise positions at ITRF2000 datum (Epoch: 2004.0) were compared against the precise positions determined at ITRF2008 datum (Epoch:.3). The results show a displacement of about 40.6 cm in NE direction between 2004.0 and.3, corresponding to a velocity of about 4.1 cm / year in NE direction. Displacements at CORS sites during 2004.0 and.3 (IGS stations constrained) The displacements can be interpreted as the tectonic movement of Arabian plate with respect to African and Asian plates. We also wanted to see the displacements / deformation within the Arabian plate as far as Saudi Arabia concerned. After fixing Riyadh CORS site in both epochs to the same value, the precise positions of 13 x CORS sites in both epochs were calculated and were compared against each other. The result can be interpreted as relative displacements within the Kingdom, only 4mm/year. XXV International Federation of The results show a displacement of about 3.2 cm between Surveyors 2004.0 Congress, and Kuala.3, corresponding to a velocity of about 4 mm / year in NE direction.

CONCLUDING REMARKS Since the mid 1980 s GNSS has been serving users throughout the world with navigation and geodetic positioning data. With the introduction of network based CORS, GNSS is now providing these services more accurately and economically. The GNSS data together with other types of data such as InSAR, seismic, etc. shall effectively serve studies related to geohazards, disaster management, and early warning. CONCLUDING REMARKS Here, very precise coordinates (mm-level precision) of 13 x GFN stations were determined in the latest ITRF2008 datum and epoch.3. Thus, once again, Saudi Arabia has very precise fiducial stations to be used as reference throughout the Kingdom. The results show that a displacement of about 40.6 cm in NE direction between 2004.0 and.3, corresponding to a velocity of about 4.1 cm / year in NE direction although relative displacements within the Kingdom is only 4 mm /year. These numbers show that the coordinates based on MTRF2000 datum has about 41 cm offset in NE direction with respect to the coordinates computed at the present with reference to IGS stations.

THANK YOU FOR YOUR ATTENTION