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GI Systems and Science January 11, 2012. Points to Cover  Introduction  Maps and spatial data  How spatial data is represented in GIS Scale Spatial.

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Presentation on theme: "GI Systems and Science January 11, 2012. Points to Cover  Introduction  Maps and spatial data  How spatial data is represented in GIS Scale Spatial."— Presentation transcript:

1 GI Systems and Science January 11, 2012

2 Points to Cover  Introduction  Maps and spatial data  How spatial data is represented in GIS Scale Spatial entities Coordinate system

3 Introduction  GIS turn spatially referenced data into information  GIS creates representations of the real world Follow some logic Simplified Selective  The simplified view of the real world is otherwise known as a model Means of getting a grip on complexity of the real world (Hardisty et al., 1993).

4 Maps and Spatial Data  GIS approach to modeling and presenting spatial data is influenced by cartography  Map a representation, normally to scale and on a flat medium, of a selection of material or abstract features on, or in relation to, the surface of the earth  Any map is a cartographic abstraction of the real world What is represented on a map and how it is represented depends on the purpose of the map Map is a communication device

5 Maps and Spatial Data Figure 2.5 Cold War propaganda map Source: Topfoto / Roger-Viollet

6 Types of Maps  Topographic Contain diverse set of data on different themes  Thematic Show data on particular theme

7 Representing Spatial Data  Scale  Spatial entities  Coordinate system  Projection

8 Scale  The ratio of a distance on a map to the corresponding distance on the ground  Can be expressed in three ways  ‘Large scale’ versus ‘small scale’

9 Scale-Related Generalization Figure 2.11 Source: Heywood et al., 2011

10 Spatial Entities  All features of the real world are represented using three basic two-dimensional models: Points Lines Polygons  The model chosen to represent a particular feature depends on the scale

11 Figure 2.10 Representing a city at different map scales Source: Reproduced by permission of Ordnance Survey on behalf of HMSO. © Crown Copyright 2011. All rights reserved. Ordnance Survey Licence number 100030901

12 Coordinate Systems  A coordinate system is used to locate features on the Earth’s surface or representation of this surface  Three categories of spatial referencing methods: Geographic coordinate systems Rectangular coordinate systems  Universal Transverse Mercator (UTM) grid Non-coordinate systems  Provide spatial reference using a descriptive code  Postal code system

13 Geographic Coordinate System  Latitude: describes how far north or south of the equator a feature is located each degree (written: 40°) is divided into 60 minutes (written: 35') and each minute into 60 seconds (written: 19"). e.g. 40° 35' 19" N  Lines of latitude = parallels Image from ArcGIS Desktop Help Copyright © Environmental Systems Research Institute, Inc.

14 Geographic Coordinate System  Longitude: denotes how far east or west of the prime meridian a feature is located e.g. 50° 27' 03" E  Lines of longitude = meridians Image from ArcGIS Desktop Help Copyright © Environmental Systems Research Institute, Inc.

15 Representing Earth’s Surface The figure courtesy of Columbia Earth Institute library website  GCS is based on the assumption that Earth is a sphere  Shape of the Earth is better represented by a spheroid (ellipsoid) Equatorial bulge Polar flattening

16 Representing Earth’s Surface  A list of most common reference spheroids The table courtesy of Wikipedia NameEquatorial axis, mPolar axis, m Inverse flattening(1/f), m Airy 18306 377 563.46 356 256.9299.324 975 3 Clarke 18666 378 206.46 356 583.8294.978 698 2 Bessel 18416 377 397.1556 356 078.965299.152 843 4 International 1924 6 378 3886 356 911.9297 Krasovsky 19406 378 2456 356 863298.299 738 1 GRS 19806 378 1376 356 752.3141298.257 222 101 WGS 19846 378 1376 356 752.3142298.257 223 563 Sphere (6371 km)6 371 000 ∞

17 Representing Earth’s Surface The figure courtesy of Columbia Earth Institute library  The Earth’s surface is not smooth and regular  Geoid is a model that gives a more accurate representation of the Earth’s surface Based on the variation in the gravity field of the Earth

18 Representing Earth’s Surface  Geoid represent the surface of the Earth at the mean sea level. © Commonwealth of Australia 2011 on behalf of ICSM, http://www.icsm.gov.au/mapping/index.htmlhttp://www.icsm.gov.au/mapping/index.html

19 Representing Earth’s Surface  A datum is a set of values that defines the position of spheroid relative to the centre of the Earth Combination of an spheroid and a geoiod

20 Representing Earth’s Surface  Types of datums Local or regional  Spheroid is positioned to fit the geoid in a particular area Geocentric  Align with the surface of a spheroid more evenly over the whole Earth © Commonwealth of Australia 2011 on behalf of ICSM http://www.icsm.gov.au/mapping/index.html


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