1. Spatial data can be described according to: entity distinct object (river) attribute characteristic of entity (discharge) relationship linkages amongst objects (drainage basin)

2. Advantages of digital maps over paper Easier to produce Easier to store Easier to distribute Dimensional stability

3. topology mathematics of spatial relationships among point, line and area objects.

4. Map a graphical representation of the spatial structure of physical and/or cultural environments

5. Map are abstractions since they present the real world in a simplified fashion at a reduced scale.

6. maps are used for: 1.the display of spatial data 2.the analysis of spatial data

7. Cartography is the art and science of map-making

8. Cartographic considerations Map scale Data classification Symbolization Generalization

9. Map scale the ratio between distances measured on a map and the corresponding distances measured on the ground

10. large scale map  displays a small area in greater detail small scale map  displays a large area in lesser detail

11. the proposed use of a map is critical in determining the scale at which it is produced

12. methods for describing map scale: Representative fraction1 : 3,500,000 Graphical (bar) Verbal“one inch equals one mile”

13. classes of maps Reference maps (general purpose) Thematic maps (special purpose)

14. Mapping process Planning stage –needs assessment –project specifications are established (cost/time) Data acquisition stage –primary data/secondary data Cartographic production stage –design –drafting –proofing –printing Product delivery stage

15. Georeferencing the representation of the location of real- world features within the spatial framework of a particular coordinate system

16. Relationship between coordinate systems and map projections Map projections define how positions on the Earth’s curved surface are transformed onto a flat map surface Coordinate systems provide a referencing framework by which positions are measured and computed.

17. Plane coordinate systems Plane rectangular system (Cartesian) Plane polar coordinates

18. Cartesian sytem (Figure 2.4) X-axis (easting) Y-axis (northing) 1 st quadrant (+x, +y) 2 nd quadrant (+x, -y) 3 rd quadrant (-x, -y) 4 th quadrant (-x, +y)

19. Plane polar coordinate system (Vector) see Figure 2.5 Polar axis = baseline Radius vector, vectorial angle Positive angles are measured in clockwise direction from polar axis

20. conversions One can convert from plane rectangular coordinate to plane polar coordinates using basic trigonometric functions

21. Geographic Coordinate System Latitudeangular distance north or south of baseline (equator) Longitudeangular distance east or west of baseline (prime meridian) graticule = grid of latitude and longitude lines (parallels and meridians) on a map or globe

22. Map projection Is a systematic representation of all or part of the surface of a round body, especially the earth, on a plane (Snyder, 1987) a two-dimensional spatial rendition of a the Earth’s surface (Fesperman, 2002)

23. Spatial properties of a map (projection) area direction distance shape

24. Projection typepreserves Equal area (equivalent)area conformal (orthomorphic)shape equidistantdistance

25. Map projection types a developable surface is one that can be laid flat without distortion (see Figure 2.11) Cylindrical Conical Planar

26. Map projection aspect Describes the orientation of the developable surface relative to the globe normalaxis of cylinder or cone parallel to earth axis transverseaxis of cylinder or cone is perpendicular to earth axis obliqueaxis oriented between normal and transverse cases

27. Map projection viewpoints Figure 2.13 Gnomonic –Light source at center of globe –Great circles are straight lines (navigation) Orthographic –Light source at infinity –Equal areas preserved Stereographic –Light source at far side of globe –Planar are conformal, cylindrical are compromised

28. see Table 2.1

29. The Ellipsoid the earth is not a sphere, but an oblate spheroid, being slight depressed at the poles satellite-based observations have allowed for the development of global standard in mathematical model

30. The Geoid reference surface for vertical coordinates (above or below the datum) equivalent to mean sea level in the earth’s oceans determined by equal gravimetric potential