An Introduction to Coordinate Systems in South Africa



Similar documents
Earth Coordinates & Grid Coordinate Systems

Lecture 2. Map Projections and GIS Coordinate Systems. Tomislav Sapic GIS Technologist Faculty of Natural Resources Management Lakehead University

The Chief Directorate: National

The Map Grid of Australia 1994 A Simplified Computational Manual

UTM Zones for the US UTM UTM. Uniform strips Scalable coordinates

EPSG. Coordinate Reference System Definition - Recommended Practice. Guidance Note Number 5

What are map projections?

The Earth Really is Flat! The Globe and Coordinate Systems. Long History of Mapping. The Earth is Flat. Long History of Mapping

WGS AGD GDA: Selecting the correct datum, coordinate system and projection for north Australian applications

GEOGRAPHIC INFORMATION SYSTEMS CERTIFICATION

SESSION 8: GEOGRAPHIC INFORMATION SYSTEMS AND MAP PROJECTIONS

World Map Lesson 4 - The Global Grid System - Grade 6+

WILD 3710 Lab 3: GIS Data Exploration Camp W.G. Williams

THE UNIVERSAL GRID SYSTEM

Geomatics Guidance Note 3

NGA GRID GUIDE HOW TO USE ArcGIS 8.x ANS 9.x TO GENERATE MGRS AND OTHER MAP GRIDS

量 說 Explanatory Notes on Geodetic Datums in Hong Kong

Measuring the Earth Using a GPS M. Scott Wilkerson & M. Beth Wilkerson, DePauw University, May 10, 2007

2 GIS concepts. 2.1 General GIS principles

WHAT YOU NEED TO USE THE STATE PLANE COORDINATE SYSTEMS

Keywords: coordinate systems, latitude, longitude, georeferencing, global positioning system, GPS, geodetic datum, ellipsoid, geocoding, postal code

Solar Angles and Latitude

UTM: Universal Transverse Mercator Coordinate System

Coordinate Systems. Orbits and Rotation

Navigation: Latitude and Longitude

Pre and post-visit activities - Navigating by the stars

Basic Coordinates & Seasons Student Guide

PLOTTING SURVEYING DATA IN GOOGLE EARTH

The Globe Latitudes and Longitudes

11.1. Objectives. Component Form of a Vector. Component Form of a Vector. Component Form of a Vector. Vectors and the Geometry of Space

A guide to coordinate systems in Great Britain

Introduction to GIS (Basics, Data, Analysis) & Case Studies. 13 th May Content. What is GIS?

GIS IN ECOLOGY: SPATIAL REFERENCING

Understanding Map Projections

Maintaining High Accuracy in Modern Geospatial Data

Data Visualization Techniques and Practices Introduction to GIS Technology

CHAPTER 9 SURVEYING TERMS AND ABBREVIATIONS

Cartographic Projections

Coordinate Conversions and Transformations including Formulas

Newton s Law of Gravity

Sun Earth Relationships

The following words and their definitions should be addressed before completion of the reading:

Full credit for this chapter to Prof. Leonard Bachman of the University of Houston

GPS LOCATIONS FOR GIS: GETTING THEM RIGHT THE FIRST TIME

Visualizing of Berkeley Earth, NASA GISS, and Hadley CRU averaging techniques

Stage 4. Geography. Blackline Masters. By Karen Devine

The Size & Shape of the Galaxy

4 The Rhumb Line and the Great Circle in Navigation

IAntarcticaI. IArctic Ocean I. Where in the World? Arctic Ocean. Pacific Ocean. Pacific Ocean. Atlantic Ocean. North America.

Using Geocoded TIFF & JPEG Files in ER Mapper 6.3 with SP1. Eric Augenstein Earthstar Geographics Web:

Geography I Pre Test #1

SECOND GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

Plotting Earthquake Epicenters an activity for seismic discovery

Chapter 4: The Concept of Area

Unit One Study Guide

Earth-Sun Relationships. The Reasons for the Seasons

The Basics of Navigation

Lines of Latitude and Longitude

GNSS and Heighting, Practical Considerations. A Parker National Geo-spatial Information Department of Rural Development and Land Reform

Understanding Map Projections

How do you find a place on a globe? How do you look up a place based on latitude and longitude?

Surveying on NAD83 State Plane Coordinate System

Latitude, Longitude, and Time Zones

CHAPTER 4 LEGAL DESCRIPTION OF LAND DESCRIBING LAND METHODS OF DESCRIBING REAL ESTATE

Gravitational potential

COASTLINING THE ZODIAC

EECS467: Autonomous Robotics Laboratory Prof. Edwin Olson. Map Projections and GPS

GIS User Guide. for the. County of Calaveras

Week 1. Week 2. Week 3

Tropical Horticulture: Lecture 2

GPS. Essentials of Satellite Navigation. Compendium. locate, communicate, accelerate. Abstract

CELESTIAL MOTIONS. In Charlottesville we see Polaris 38 0 above the Northern horizon. Earth. Starry Vault

TerraColor White Paper

Searching Land Records thru the BLM General Land Office Records.

Which month has larger and smaller day time?

Tax Parcel Mapping. Visual Representations of Legal Descriptions and So Much More

Creating Figure Ground Maps in ArcMap 10.x: Basic procedures to download, open, manipulate and print spatial data

Introduction to CATIA V5

CONTENTS. Page 3 What is orienteering? Page 4 Activity: orienteering map bingo. Page 5 Activity: know your colours. Page 6 Choosing your compass

Section. Tolerances. Aluminum Extrusion Manual. 4th Edition

6. The greatest atmospheric pressure occurs in the 1) troposphere 3) mesosphere 2) stratosphere 4) thermosphere

Anamorphic Projection Photographic Techniques for setting up 3D Chalk Paintings

CELESTIAL CLOCK - THE SUN, THE MOON, AND THE STARS

Objectives After completing this section, you should be able to:

Metadata for Big River Watershed Geologic and Geomorphic Data

Stellarium a valuable resource for teaching astronomy in the classroom and beyond

Institute of Natural Resources Departament of General Geology and Land use planning Work with a MAPS

Section 4: The Basics of Satellite Orbits

U.K. OFFSHORE OPERATORS ASSOCIATION (SURVEYING AND POSITIONING COMMITTEE) UKOOA DATA EXCHANGE FORMAT P6/98 DEFINITION OF 3D SEISMIC BINNING GRIDS

Orientation to the Sky: Apparent Motions

Getting Land Survey Vertical & Horizontal Control via the Internet

Where in the World is the arctic?

CATIA Wireframe & Surfaces TABLE OF CONTENTS

Optical Illusions Essay Angela Wall EMAT 6690

Flight and Orbital Mechanics

The Sphere of the Earth Description and Technical Manual

Transcription:

An Introduction to Coordinate Systems in South Africa Centuries ago people believed that the earth was flat and notwithstanding that if this had been true it would have produced serious problems for mariners sailing off to explore the world it would nevertheless have made life a lot simpler for surveyors in preparing maps. Unfortunately for us the earth is an irregular shape which is roughly spherical. The figure below illustrates this irregularity (land areas in green and seas in blue). Model of the Earth A.Mitchell Surveying & Land Information Dept (October 2011) Surface of the Earth Land Sea Geoid Ellipsoid Mathematicians need to define a theoretical surface on which to base calculations. The figure most commonly used is the ellipsoid (imagine a sphere which has been flattened at the poles). This is represented on the figure to the left by a red dotted line. You can see this polar flattening in the globe on the right Once an ellipsoid has been defined, lines of latitude and longitude can be generated for that ellipsoid. Lines of longitude are great circles which pass through both the north and south poles. 0 longitude passes through the Greenwich observatory in London, England. Values of longitude (0 to 360 ) in an easterly direction around the globe. Longitude 31 east passes directly through Durban (and also Harare in Zimbabwe and Cairo in Egypt). Lines of latitude are defined a right angles to lines of longitude. The largest such line is equidistant from both the north and south poles and is defined as the equator at 0 latitude. Values north of the equator positively to 90 at the north pole and values south of the equator positively to 90 at the south pole (southerly latitude values sometimes are given negative values). latitude North + longitude Equator West - East + South - Prime meridian page 1 of 5

It is important to note that values of latitude & longitude are angles subtended from the centre of the defined ellipsoid and as such are complicated to work with for survey calculations. The vast majority of maps and plans are two dimensional and what is needed are values which define two dimensional position - for example values of Y and X. To do this, ellipsoidal values need to be projected onto a plane surface using simple shapes as illustrated below. The type of projection chosen is dependant on the shape and position of the area to be mapped. The idea is to project with minimum distortion but we must understand that no projection will be perfect - imagine pealing an orange and trying to press the peal onto a flat surface without tearing it. A common type of projection used world wide is the Transverse Mercator Projection. It is a variation of the cylindrical projection shown above but the imaginary cylinder is positioned in contact with a defined line of longitude. You can see from the illustration below right that distortion occurs both east and west of this defined line of longitude. page 2 of 5

THE UNIVERSAL TRANSVERSE MERCATOR PROJECTION (UTM) This is an internationally used projection system. The globe is divided into sixty zones each 6 wide. The imaginary cylinder is progressively positioned over the mid point of each zone to create a series of coordinate systems. There is still a bit of distortion so a scale factor is applied to all calculations to try and minimize this. SOUTH AFRICA S NATIONAL COORDINATE SYSTEM In South Africa, a variation of the UTM projection called the Gauss Conformal Projection is used to define our national coordinate system. The principles of the projection are the same but each zone is only 2 wide (as opposed to 6 wide). There is less distortion and no scale factor is required. Longitudes 17 East, 19 East, 21 East, 23 East, 25 East, 27 East, 29 East, 31 East and 33 East are used as the mid-points of each 2 projection. These coordinate zones were referred to as Lo17, Lo19, Lo21..etc (Cape Datum) until 1999 when the national system changed from one based on the Clarke 1880 modified ellipsoid to the more internationally recognised WGS84 ellipsoid. The coordinate zones are now referred to as Wg17, Wg19, Wg21..etc (Haartebeeshoek 1994 datum). The coordinate zone in use in the Durban area is Wg31 because as mentioned earlier, longitude 31 east runs directly through the city. page 3 of 5

THE NATIONAL COORDINATE SYSTEM USED IN THE DURBAN AREA Directions Angles of direction positively in a clockwise direction. The direction 0 points south Programmes such as ArcView interpret Y and X values in UTM orientation as shown below in blue. This is why coordinates in our National System have to appear reversed and of opposite sign in order for their relative positions to be viewed correctly in ArcView. ie X(ArcView) = -Y(wg31) and Y(ArcView) = -X(wg31) PTO for more... Distortions Distortion s with distance away from the central meridian (longitude 31 east).this affects both distance and direction measurements. Corrections have to be applied to their values to enable accurate calculations of both Y and X coordinates. page 4 of 5

Northings (Y values) THE EFFECT ON SOUTH AFRICAN NATIONAL SYSTEM COORDINATES WHEN USED IN INTERNATIONAL SOFTWARE ie ArcView, Auto- Cad etc Equator SOUTH AFRICAN COORDINATE SYSTEM Northings (or Y coordinates) to the north Origin (0,0) Y values X values Y coordinates positively to the west SOUTH AFRICAN NATIONAL COORDINATE SYSTEM UTM COORDINATE SYSTEM UTM Longitude of zone origin. (31 East in Durban area) Eastings (X values) Eastings (or X coordinates) to the east X coordinates positively to the south Note : For correct Y and X grid coordinates, multiply both values by 1 International software such as the ESRI products (ArcGIS etc) and AutoDesk products (AutoCad etc) interpret coordinate values in Universal Transverse Mercator (UTM) orientation as shown in blue to the left. UTM values are referred to as Eastings and Northings (X s & Y s). South African National Coordinates (SA) are referred to as Y s and X s. If our SA values are simply entered without correction, then the software will interpret our Y s as Northings and our X s as Eastings ie Y values(sa) are read as Y values (UTM) and are therefore increasing positively northwards instead of westwards AND X values(sa) are read as X values (UTM) and are therefore increasing positively eastward instead of southward - all relative to the coordinate origin which is the Equator and the central meridian of the coordinate zone (which in the Durban area is longitude 31 East). It may be possible in some software to enter the necessary predefined coordinates systems within coordinate settings options, but if not, in order to view South African National Coordinate System values in their correct relative positions, it is necessary to enter their values as follows: X value (UTM) = Y value (SA) x( 1) Y value (UTM) = X value (SA) x( 1) Although relative position is now correct, It should be noted that the displayed coordinates will still have opposite signs and maps produced with grid values will reflect this as seen on the map to the left. All maps produced using this software and displaying coordinate grid values, should therefore include an explanatory note referring to this. An example appears on the map to the left. ArcView ver10 now has settings which enable South African system coordinates and grid values to be viewed correctly but be aware that all datasets used in GIS software should have coordinate systems defined. If not, they may not display correctly. Should anyone require advice or clarity on any aspect of the use of coordinates in general, please do not hesitate to contact the writer or the Land Surveying Branch of the Surveying & Land Information Department. page 5 of 5