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1 Development of Geodetic GPS Infrastructure and Its Development of Geodetic GPS Infrastructure and Its Applications: The Malaysia Experience Applications: The Malaysia Experience Abd Majid.A.Kadir, Shahrum Ses, Kamaluddin Omar & Abdullah Hisam Omar Fac. of Geoinformation Science and Eng. Universiti Teknologi Malaysia Seminar On GPS Dubai, United Arab Emirates 22 nd July 2003 Kadir Taib, Teng Chee Hua, Azhari Mohamed, Chang Leng Hua & Soeb Nordin Dept. of Surveying & Mapping Malaysia, Kuala Lumpur BY Summary of Presentation: 1. 1. Introduction Introduction 2. 2. Classical Geodetic Infrastructure Classical Geodetic Infrastructure 3. 3. Modern Geodetic Infrastructure Modern Geodetic Infrastructure 4. 4. Development of Geocentric Datum for Malaysia Development of Geocentric Datum for Malaysia GDM 2000 GDM 2000 5. 5. Applications Applications 6. 6. Future Directions Future Directions 7. 7. Conclusion Conclusion

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Development of Geodetic GPS Infrastructure and Its Development of Geodetic GPS Infrastructure and Its

Applications: The Malaysia Experience Applications: The Malaysia Experience

Abd Majid.A.Kadir, Shahrum Ses, Kamaluddin

Omar & Abdullah Hisam Omar

Fac. of Geoinformation Science and Eng.

Universiti Teknologi Malaysia

Seminar On GPS

Dubai, United Arab Emirates

22nd July 2003

Kadir Taib, Teng Chee Hua, Azhari Mohamed,

Chang Leng Hua & Soeb Nordin

Dept. of Surveying & Mapping Malaysia,

Kuala Lumpur

BY

Summary of Presentation:

1.1. IntroductionIntroduction

2.2. Classical Geodetic InfrastructureClassical Geodetic Infrastructure

3.3. Modern Geodetic InfrastructureModern Geodetic Infrastructure

4.4. Development of Geocentric Datum for Malaysia Development of Geocentric Datum for Malaysia

GDM 2000 GDM 2000

5.5. ApplicationsApplications

6.6. Future Directions Future Directions

7.7. ConclusionConclusion

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South East Asia

South East Asia region consists of

ten (10) countries:

1) Malaysia

2) Singapore

3) Indonesia

4) Philippines

5) Brunei

6) Cambodia

7) Vietnam

8) Thailand

9) Laos

10)Burma/Myanmar

South East Asia Region

Introduction

Malaysia Introduction

Geography

Area: 329,749 sq. km Terrain: Coastal plains and interior,

jungle-covered mountainsClimate: Tropical. The South China Sea separates

Peninsular Malaysia from EastMalaysia on Borneo (640 km.).

Government

Independence: August 31, 1957Subdivisions: 13 states and three federal territories (Kuala Lumpur, Labuan Island,Putrajaya federal administrative territory)People

Nationality: Malaysian.Population (2000): 23.3 million.

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Malaysia: Topographic VisualizationIntroduction

Highest Point in Peninsular Malaysia: Mt. Tahan (2,187 m)

Highest Point in East Malaysia : Mt. Kinabalu (4,101 m)

Mt. Tahan, Pahang

Mt. Kinabalu, Sabah

Department of Surveying and Mapping Malaysia (DSMM): Profile

Introduction

The Past in Brief

1885:The history of the Department of Survey and Mapping Malaysia(DSMM) began with the establishment of theJohor Survey Department and the Perak

Trigonometrical Survey Department.

1909:The formation of the Malay States Survey Department (Federated Malay States).

1946:

All state Survey Departments were unified under one single administration headed by the Surveyor-General.

1982:The integration of JUPEM under the Ministry of

Land and Regional Development (Ministry of Land and Cooperative Development).

Present:Modern Data Provider

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Introduction

The Department Role

To provide efficient and high quality survey and mapping services and a

geographical information dissemination system suitable for national requirements

MISSION

Classical Geodetic Infrastructure

Triangulation Network of Peninsular Malaysia

Malaysia Revised Triangulation

(MRT)

� MRT has been used for geodetic, mapping, cadastral and several other activities since 1948 in Peninsular Malaysia

� MRT network consists of 77 geodetic, 240 primary, 837 secondary and 51 tertiary

stations.

1/300.8017Flattening (f)5

6,377,304.063Semi-major axis (a)3

Kertau, PahangOrigin2

Modified EverestReference Ellipsoid1

MRTParameterNo.

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Borneo Triangulation (BT68)

�Timbalai Datum - Separate Network from

Pen.Malaysia.

� Still used for geodetic, mapping and surveying

Triangulation Network of East Malaysia

1/300.8017Flattening (f)5

6,377,298.565Semi-major axis (a)3

Timbalai,SarawakOrigin2

EverestReference Ellipsoid1

BT68ParameterNo.

Classical Geodetic Infrastructure

Malaysia Active GPS System (MASS)

Modern Geodetic Infrastructure

� Malaysia Active GPS System consistent of 15 permanent GPS stations, which track GPS satellites at an

attitude of 20,000 km away in space and allow users in Malaysia to have 24 hour access of GPS data.

� These stations are strategically located throughout the country .

Objectives

� To enable DSMM to carry out surveying and mapping functions more effectively.

� To maintain the National Reference Frame System at centimetre accuracy.

� To monitor and provide the user community with a coordinate system that is connected to the national and

global reference frame.

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� Established in 1994 and provide a

consistent set of coordinates in the

WGS84 datum (PMPGN95).

� The network consists of 238 GPS

stations with an average spacing of

about 30km.

� Strengthening and readjustment of

PMPGN95 to [email protected] :

PMPGN2000

� The horizontal accuracy of the

PMPGN2000 are 1-2 part per million

(ppm) and 3 to 5 ppm for vertical

component

Modern Geodetic Infrastructure

Peninsular Malaysia Primary Geodetic GPS Network (PMPGN)

Existing PMPGN95

Modern Geodetic Infrastructure

� Established in 1997 and provide a

consistent set of coordinates in the

WGS84 datum (EMPGN97).

� The network consists of 171 GPS

stations with an average spacing of

about 30km.

� Strengthening and readjustment of

EMPGN97 to [email protected] :

EMPGN2000

� The horizontal accuracy of the

EMPGN2000 are 1-2 part per million

(ppm) and 3 to 5 ppm for vertical

componentExisting EMPGN97

East Malaysia Primary Geodetic GPS Network (EMPGN)

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First Order GPS Network of East Malaysia

� Historically, Malaysian geodetic datums has been established since 19th century

using conventional surveying techniques and procedures

� Confined to small areas of the globe, fit to limited areas and to satisfy national

mapping requirements.

� Local datums are not aligned with global geocentric coordinates frames.

� Existing datum not compatible with the wide spread use of satellite positioning

systems and international recommendation.

� Two separate geodetic datums ( Peninsular Malaysia and East Malaysia)

Development of Geocentric Datum for

Malaysia GDM2000

Problems With Classical Datum

� GPS Data Collection (MASS stations, 1999-2002)

� The data processing and adjustment of the MASS network

� Computation of the new geocentric datum coordinates at specific epoch.

� Determination of velocity model

� Strengthening and readjustment of Peninsular Malaysia Geodetic GPS Network

(PMPGN95) and East Malaysia GPS Geodetic Network (EMPGN97)

� Transformation parameter computation.

Realisation of GDM2000

Implementation of Geocentric Datum

GDM 2000

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Processing and Adjustment of MASS Network (1999-2002)

� Internal Accuracy:

• 1.7 –2.0 mm horizontal

• 4.4 mm height

� Final Adjustment accuracy:

• 3-16 mm horizontal

•8-13 mm height

� Final Coordinates: [email protected]

GDM 2000

Strengthening and Readjustment of PMGSN and EMGSN

� To provide control in GDM datum

� GPS campaign: Oct-Nov 2000

� 36 stations observed

� Connecting to MASS network

� New PMPGN and EMPGN with ITRF2000 control coordinates

GDM 2000

99.5 100 100.5 101 101.5 102 102.5 103 103.5 104 104.5

2

3

4

5

6

7

GP50

GP58 GP84

GP18

GP24

P102

P281

P310 P247

GP36

P219 P258

P221

P238

P229

GP32

P290

P298 P299

GP02

P213

GP47 GP43

GP52

GP37

GP21

P297 P244

P263 P274

P255

GP28

GP06

M331

GP98

GP54

UTMJ

KTPK

IPOH

KUAN

GETI

ARAU

USMP

Strengthening of PPGN

KUAL

Mass Station

Main Station

Check Station

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0.246403 ppm

-0.004068 arc sec

-0.027860 arc sec

0.036955 arc sec

2.129729

-1.936201

1.626737

PARAMETER

SCALE

RZ

RY

RX

DZ

DY

DX

COMPONENT

1.6 x 10-8

8.4 x 10-9

1.3 x 10-8

8.3 x 10-9

0.2878

0.2404

0.3207

STD. DEV

Transformation Parameter : PMPGN95 – GDN2000

GDM 2000

CCDB : Geocentric Based Cadastral Control Database

SDCDB: State Digital Cadastral DatabaseNDCDB : National Digital Cadastral Database ( Geocentric)

NDCDB

SDCDB

DATA

SELECTION

ADJUSTMENT

TRANSFORM

QUALITYCONTROL

CCDB

TEMPNDCDB

EDITING

Automated Database Conversion System

Input

Connection

Lines

DATA INTEGRITY

CHECK

Applications

Digital Cadastral System

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Zero Order Geodetic GPS

Network (MASS Stations)

First Order Geodetic GPS

Network (30km Network)

Cadastral Control Infrastructure

•10km,2.5km,0.5km

•Ties to Cadastral Network

Computation of Geocentric Cassini

& RSO

Coordinates

Cadastral Control

Database

CCDB

Design & Analysis Of

CCDB

Digital Cadastral System

The Cadastral Control Development Methodology

Applications

Applications

Primary Grid

Secondary Grid

GPS Control

GPS Control

GPS Control Network

Geocentric Based Cadastral Control Infrastructure

Geocentric Based Cadastral Control Database Cadastral Network Adjustment Based On Geocentric Datum

Digital Cadastral System

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Methodology of Georeferencing

GEO-REFERENCING

CAMS/DTDB

(RSO)LOCAL

NDTDB

(RSO)GEOCENTRIC

NDCDB

(RSO)GEOCENTRIC

INTEGRATION

ISSUES ANALYSIS

a. POLYNOMIAL TRANSFORAMTION

(by graphic)

b. DATUM TRANSFORMATION

(by point)

Applications

Mapping: Georeferencing Topographic Data to

Geocentric Datum

2D Reverse

Transformation using RSO formulae

3D Transformation using Bursa Wolf parameter model

[ N, E ][ N, E ]RSORSO[ LAT, LON ][ LAT, LON ]MRTMRT

[ LAT, LON ][ LAT, LON ]WGS84WGS84[ N, E ][ N, E ]RSORSO 2D Direct Transformation using

modified RSO parameterDestination Datum

Local

Geocentric

Datum Transformation Procedure

Applications

Mapping: Georeferencing Topographic Data to

Geocentric Datum

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Applications

Mapping: Georeferencing Topographic Data to Geocentric Datum

� Coordinates change of approx. 200 m

� Simple transformation process for mapping product but need dense GPS

network for a higher accuracy fit.

� Change in coordinates of map features

• 1: 50,000 --- 4 mm on the map• 1:10,000 --- 20 mm on the map

� Future mapping product will be base on GDM 2000

MSL height was derived from the ellipsoidal heights using the following formula:

H = h – N

Where

H = Orthometric / MSL height derived from GPS/EGM96

h = Ellipsoidal (GPS) height

N = Geoid height (based on EGM96 Geoid Model)

GPS LevellingApplications

GPS Levelling Concept

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GPS LevellingApplications

Principle of Airborne Gravimetry System

GPS Levelling

Airborne Gravimetry Flight Paths

Applications

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GPS Levelling

Geoid of Sarawak and Sabah from downward continued gravity.

Applications

106 108 110 112 114 116 118 120

0

2

4

6

8

Fleet Navigation Applications

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Applications

Hydrographic Surveying

Airborne Photography

Applications

Photo Control

Kuala Lumpur Base Map

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Intelligent Transportation SystemApplications

Petroleum CompanyApplications

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Electric Power Supply CompanyApplications

Control Station For Hydroelectric Dam Hydroelectric Dam

Telecommunication CompanyApplications

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Precision Farming

Applications

Mapping: GIS ApplicationsApplications

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Future DirectionsApplications

� Development of GPS RTK Network for Sabah & Sarawak (SSRTK Net) –

2004/2005

•Sparse network: 18 stations covering the whole Sabah & Sarawak

• Two denser : covering Kuching and Kota Kota Kinabalu

� Development of GPS RTK Network for Peninsular Malaysia (PMRTK Net) –

2003/2004

• Sparse network: 20 stations covering the whole Peninsular Malaysia

•Two denser : covering Kuala Lumpur and Penang