GPS Remote Sensing. GIS Photogrammetry. GEODESY Equipment (total station) CARTOGRAPHY Survey Software. Map Projection Coordinate Systems

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GPS Remote Sensing GIS Photogrammetry GEODESY Equipment (total station) CARTOGRAPHY Survey Software Map Projection Coordinate Systems 1

Coordinate Systems, Datum and Map Projection Dr. Maher A. El-Hallaq Lecturer of Surveying The Islamic University of Gaza

Every map user and maker should have a basic understanding of projections no matter how much computers seem to have automated the process. - John P. Snyder 3

Why is this important? Creating spatial data (collecting GPS data) Import into GIS and overlay with other layers Acquiring spatial data from other sources Display your GPS data using maps 4

Coordinate Systems There are 2 types of coordinate systems: Geocentric Coordinate System رزي ادات ظم Geographic Coordinate Systems ظم ادات را Projected Coordinate Systems ظم ادات ط 5

Geocentric Coordinate System 6

Geographic Coordinate System - Earth is not a sphere - Poles are flattened - Bulges at equator Earth is ellipsoid or a spheroid 7

Geographic Coordinate System Ellipsoid approximates the shape of the earth Model of the earth Also called an spheroid 8

Geographic Coordinate System Reference Ellipsoid Equatorial Reciprocal a (m) f 10 4 Radius a (m) Flattening 1/f with WGS84 with WGS84 Airy 1830 6377563.396 299.3249646 573.604 0.11960023 Clarke 1866 6378206.4 294.9786982-69.4-0.37264639 Clarke 1880 6378249.145 293.465-112.145-0.54750714 Everest 6377276.345 300.8017 860.655 0.28361368 GRS 1967 6378160.0 298.247167427-23.0-0.00113048 GRS 1980 6378137.0 298.257222101 0.0-0.00000016 Helmert 1906 6378200.0 298.3-63.0 0.00480795 International 6378388.0 297.0-251.0-0.14192702 Modified Everest 6377304.063 300.8017 832.937 0.28361368 South America69 6378160.0 298.25-23.0-00081204 WGS 60 6378165.0 298.3-28.0 0.00480795 WGS 66 6378145.0 298.25-8.0-0.00081204 WGS 72 6378135.0 298.26 2.0 0.0003121057 WGS 84 6378137.0 298.257223563 0.0 0.0 9

Geographic Coordinate System A datum defines the position of the ellipsoid relative to the center of the earth Origin and orientation of latitude and longitude lines are determined by the datum Hundreds of datums customized for different parts of the world 10

Geographic Coordinate System A reference system using latitude and longitude to define the location of points on the surface of an Ellipsoid (φ, λ, h) decimal degrees (DD) -92.5 degrees/minutes/seconds (DMS) 31 25 10 E Example: A location of a point in Khan Younis: φ = 31 20 N λ = 34 20 E h = 78.454 m 11

Common Datums Datum Ref. Ellipsoid X (m) Y (m) Z (m) S (ppm) ε x ε y ε z WGS84 WGS84 0.0 0.0 0.0 0.0 0.0 0.0 0.0 WGS72 WGS72 0.0 0.0 4.5 0.227 0.0 0.0-0.554 Adindan Clarke 1880-166 - 15 204 0.0 0.0 0.0 0.0 PZ1990 PZ-90 0.0 0.0 1.0 0.0 0.0 0.0-0.2062648 Ain El-abd 70 International - 150-251 -2 Egypt International - 130-117 - 151 Old Egyptian Helmert 1906-130 110-13 Qatar National International - 128-283 22 Zeros Oman Clarke 1880-346 -1 224 TOKYO Bessel 1841-148 507.5 685 12

Transforming between datums GPS GIS Special software Develop your tool Step 1 Step 2 Step 3 13

Geographic Coordinate System Universal Coordinate System (lat/lon) Lat/lon good for locating positions on surface of a globe Lat/lon is not efficient for measuring distances and areas! Latitude and longitude are not uniform units of measure One degree of longitude at equator = 111.321 km (Clarke 1866 ellipsoid) One degree of longitude at 60 latitude = 55.802 km (Clarke 1866 ellipsoid) 14

Projected Coordinate Systems A map projection is the systematic transformation of locations on the earth (latitude/longitude) to planar coordinates The basis for this transformation is the geographic coordinate system (which references a datum) Map projections are designed for specific purposes 15

Map Projection Equator International Date o Line - 0 16

Map Projection 17

This process of flattening the earth will cause distortions in one or more of the following spatial properties: Shape Conformal map projections preserve shape Area Equal area map projections preserve area Distance/Scale Equidistant map projections preserve distance Direction/Angle Azimuthal map projections preserve true direction 18

Map Projection Latitude of Origin Central Meridian False Easting False Northing Scale Factor عناصر الا سقاط الخمسة: 19

Projected Coordinate Systems Datum name Ellipsoid Projection Old Palestine Grid (OPG) Clarke 1880 modified a = 6378300.789 m 1/f = 293.466 b = 6356566.412 m Type: Cassini Soldner Latitude of Origin: 31 44 02.749 N Central Meridian: 35 12 43.490 E False Northing: 1126867.909 m False Easting: 170251.555 m Scale: 1.0 20

Mercator Projection 21

Universal Transverse Mercator (UTM) Developed by military Grid system Earth divided into 60 zones Great for small areas minimal map distortion distortion greater at edge of zones Most common map projection used 22

Universal Transverse Mercator- UTM Grid 23

Universal Transverse Mercator- UTM Grid 24

Projection Transformation 25

Transforming between Coordinates GPS GIS Special software Develop your tool 26

When GPS points don t align with GIS Data Most likely a projection issue if: There are huge errors data points do not overlay Features could be displayed in wrong state or hemisphere! 27

When GPS points don t align with GIS Data Possibly a datum issue if: GPS data overlays with GIS data, but off by several hundred feet Differences between NAD27 and NAD83 can be as much as 500 feet This creates problems when doing analysis 28

A point latitude φ, longitude λ and altitude h are (41 15 N, 75 10 E, 312.4 m). Find the geocentric coordinates of this point using WGS 84 Datum? 29

30

Thank You!!! 31