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Introduction to Geographic Information Systems Spring 2013 (INF 385T-28437) Dr. David Arctur Lecturer, Research Fellow University of Texas at Austin Lecture 5 February 7, 2013 Spatial Reference Systems, Data Sources
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Outline Models of the Earth Map projections Coordinate systems GIS data sources Vector data formats Raster data formats 2 INF385T(28437) – Spring 2013 – Lecture 5
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Models of the Earth’s shape Sphere with radius of ~6378 km Ellipsoid (or Spheroid) with equatorial radius (semimajor axis) of ~6378 km and polar radius (semiminor axis) of ~6357 km Difference of ~21km usually expressed as “flattening” (f) ratio of the ellipsoid: f = difference / major axis = ~ 1/300 for Earth and “inverse flattening” would be ~300 3 INF385T(28437) – Spring 2013 – Lecture 5
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Ellipsoid dimensions and flattening 4 INF385T(28437) – Spring 2013 – Lecture 5 Ellipsoid = Spheroid in GIS…
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Ellipsoid vs Geoid vs Datum The Geoid is approximately where sea level would be throughout the world (measured by plumb bob away from coastal areas) Due to variations in the Earth’s gravity field, this “global sea level” would not fit any one ellipsoid, as evident in figure Datum = shape of ellipsoid AND location of origin for axis of rotation relative to Earth center of mass
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Horizontal Control Datums Commons North American Datums NAD27 (1927 North American Datum) Clarke (1866) ellipsoid, non-geocentric (local origin) for axis of rotation NAD83 (1983 North American Datum) GRS80 ellipsoid, geocentric origin for axis of rotation WGS84 (1984 World Geodetic System) WGS84 ellipsoid, geocentric, nearly identical to NAD83 Other datums are also in use globally 6 INF385T(28437) – Spring 2013 – Lecture 5
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Datum shifts 7 INF385T(28437) – Spring 2013 – Lecture 5
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Datum transformations Theoretical method: use equations relating Lat/Lon in one datum to another Empirical method: use grid of differences to convert values directly from one datum to another See Esri digital book on Map Projections for more information 8 INF385T(28437) – Spring 2013 – Lecture 5
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MAP PROJECTIONS How do we get from 3D Earth to 2D maps??? 9 INF385T(28437) – Spring 2013 – Lecture 5
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Latitude and longitude Longitude (meridians) 10 INF385T(28437) – Spring 2013 – Lecture 5
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Latitude and longitude Latitude (parallels) 11 INF385T(28437) – Spring 2013 – Lecture 5
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Latitude and longitude ° Longitude (prime meridian) 0 ° Latitude (equator) 0 12 INF385T(28437) – Spring 2013 – Lecture 5
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Latitude and longitude Pittsburgh, PA USA -80 40 Coordinates 13 INF385T(28437) – Spring 2013 – Lecture 5
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Lat/Long coordinates Degrees, minutes, and seconds (DMS): 40° 26′ 2″ N latitude -80° 0′ 58″ W longitude Decimal degrees (DD) 1 degree = 60 minutes, 1 minute = 60 seconds 40° 26′ 2″ = 40 + 26/60 + 2/3600 = 40 +.43333 +.00055 = 40.434° 14 INF385T(28437) – Spring 2013 – Lecture 5
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Lat/long coordinates Translated to distance World circumference through the poles is 24,859.82 miles, so for latitude: 1° = 24,859.82 / 360 = 69.1 miles 1′ = 24,859.82 / (360 * 60) = 1.15 miles 1″ = 24,859.82 * 5,280 / (360 * 3,600) = 101 feet Length of the equator is 24,901.55 miles 15 INF385T(28437) – Spring 2013 – Lecture 5
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Picking a projection … [or: how big do you like Greenland?] 16 INF385T(28437) – Spring 2013 – Lecture 5
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Most-used methods 17 INF385T(28437) – Spring 2013 – Lecture 5
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Still more distinctions among projections 18 INF385T(28437) – Spring 2013 – Lecture 5
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Mercator projection (1569) Conformal projection Cylindrical Parallels and meridians at right angles Linear scale is constant in all directions around any point Preserves angles and shapes of small objects Distorts the size and shape of large objects Map projection for nautical purposes 19 INF385T(28437) – Spring 2013 – Lecture 5
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Hammer – Aitoff (1882-1889) Equal-area Modified azimuthal projection Good for population density (world area) Difficult to see some areas 21 INF385T(28437) – Spring 2013 – Lecture 5
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Robinson projection (1961) Pseudocylindrical Neither equal area nor conformal Meridians curve gently, avoiding extremes Good compromise projection for viewing entire world Used by Rand McNally since the 1960s and by the National Geographic Society (1988 and 1998) 22 INF385T(28437) – Spring 2013 – Lecture 5
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Albers Equal Area Conic projection Scale and shape are not preserved, distortion is minimal between the standard parallels Standard projection for British Columbia, U.S. Geological Survey, U.S. Census Bureau 24 INF385T(28437) – Spring 2013 – Lecture 5
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Other map projections… 25 INF385T(28437) – Spring 2013 – Lecture 5 http://xkcd.com/977/ http://www.watermanpolyhedron.com/maps
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And the ever-popular… 26 INF385T(28437) – Spring 2013 – Lecture 5 Bovine projection(s) Spilled Coffee Projection
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Projection important for… Measurements used to make important decisions Comparing shapes, areas, distances, or directions of map features Feature and image themes are aligned Los Angeles New York Los Angeles New York Projection: Mercator Distance: 3,124.67 miles Projection: Albers equal area Distance: 2,455.03 miles Actual distance: 2,451 miles 27 INF385T(28437) – Spring 2013 – Lecture 5
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Projection not important for… Business applications Not of critical importance Concerned with the relative location of different features Large scale maps — street maps Distortion may be negligible Map covers only a small part of the earth’s surface 28 INF385T(28437) – Spring 2013 – Lecture 5
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COORDINATE SYSTEMS Lecture 5 29 INF385T(28437) – Spring 2013 – Lecture 5
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Geographic Coordinate System (GCS) Spherical coordinates Angles of rotation of a radius anchored at earth’s center Latitude and longitude Census Bureau TIGER files 30 INF385T(28437) – Spring 2013 – Lecture 5
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U.S. Census GCS example 31 INF385T(28437) – Spring 2013 – Lecture 5
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Rectangular coordinate system Used for locating an intersection on a flat sheet of graph paper or a flat map Cartesian coordinates (x,y) State plane and UTM 32 INF385T(28437) – Spring 2013 – Lecture 5
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State Plane coordinates Established by the U.S. Coast and Geodetic Survey in 1930s Originally North American Datum (NAD 1927) More recently NAD 1983 and 1983 HARN Used by local U.S. governments All positive coordinates in feet (or meters) 33 INF385T(28437) – Spring 2013 – Lecture 5
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State Plane zones 125 zones At least one for each state Cannot have zones joined to make larger regions Follow state and county boundaries Each has its own projection: Lambert conformal projection for zones with east-west extent Transverse Mercator projection for zones with north-south extent 34 INF385T(28437) – Spring 2013 – Lecture 5
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State Plane zones 35 INF385T(28437) – Spring 2013 – Lecture 5
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State Plane zones 36 INF385T(28437) – Spring 2013 – Lecture 5
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Pittsburgh neighborhoods as state plane coordinates 37 INF385T(28437) – Spring 2013 – Lecture 5
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Universal Transverse Mercator (UTM) Rectangular coordinate system Used by U.S. military Covers entire world Metric coordinates Longitude zones are 6° wide Latitude zones are 8° high 38 INF385T(28437) – Spring 2013 – Lecture 5
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Coordinate system summary Geographic coordinate system U.S. Census State plane coordinate system Local governments U.S. military Projections defined in ArcCatalog or ArcMap (.prj) files First file added in a map document sets the projection (others will adjust to it as long as they have a.prj file) 39 INF385T(28437) – Spring 2013 – Lecture 5
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GIS DATA SOURCES We had to go through all that, so we can understand issues around importing spatial data from… 40 INF385T(28437) – Spring 2013 – Lecture 5
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GIS data sources ESRI U.S. Census USGS and other government sources GDT Dynamap/2000 U.S. Street Data Engineering companies land surveys, aerial photos, CAD drawings University Web sites (e.g. Penn State’s PASDA) Zillions of others… 41 INF385T(28437) – Spring 2013 – Lecture 5
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GIS data sources 30+ million Internet search results type “GIS data download” or “population China.e00 add the name of the state, county, or city to the search 42 INF385T(28437) – Spring 2013 – Lecture 5
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GIS departments Web sites Washington, D.C. dcgis.dc.gov/ Chicago, IL www.cityofchicago.org/gis Austin, TX Tip: Search by county name (Travis County, Texas) http://www.austintexas.gov/development/ ftp://ftp.ci.austin.tx.us/GIS-Data/Regional/coa_gis.html 43 INF385T(28437) – Spring 2013 – Lecture 5
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ESRI’s Web site http://www.esri.com/data/esri_data/demographic-overview http://www.esri.com/data/esri_data/demographic-overview 44 INF385T(28437) – Spring 2013 – Lecture 5
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U.S. Census Bureau Started building a map infrastructure in the late 1970s and early 1980s Census mapping needs were twofold: To assign census employees to areas of responsibility, covering the entire country and its possessions To report and display census tabulations by area, officials determined that the smallest area needed for these purposes is a city block or its equivalent 45 INF385T(28437) – Spring 2013 – Lecture 5
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U.S. Census Bureau Compiles all line features used to create a block layer for the entire country Map features smaller than are the responsibility of local governments deeded land parcels buildings street curbs parking lots others? 46 INF385T(28437) – Spring 2013 – Lecture 5
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Census TIGER/Line files Topologically Integrated Geographic Encoding and Referencing files Census Bureau’s product for digital mapping of the U.S. Available for the entire U.S. and its possessions Include the following geographic features roads and street centerlines railroads rivers lakes census statistical boundaries 47 INF385T(28437) – Spring 2013 – Lecture 5
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TIGER census tracts Statistical boundary (below county level) between 1,000 and 8,000 people (in general) 1,700 housing units or 4,000 people homogeneous population characteristics (economic status and living conditions) normally follow visible features may follow governmental unit boundaries and other nonvisible features more than 60,000 census tracts in Census 2000 Also, the legal basis for developing congressional districts 48 INF385T(28437) – Spring 2013 – Lecture 5
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PA tracts 49 INF385T(28437) – Spring 2013 – Lecture 5
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Allegheny County tracts 50 INF385T(28437) – Spring 2013 – Lecture 5
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Pittsburgh tracts 51 INF385T(28437) – Spring 2013 – Lecture 5
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TIGER census block groups Subdivision of a census tract 400 housing units, with a minimum of 250 and a maximum of 550 housing units Follow clearly visible features such as roads, rivers, and railroads 52 INF385T(28437) – Spring 2013 – Lecture 5
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Census block groups 53 GIS TUTORIAL 1 - Basic Workbook
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TIGER census blocks Smallest geographic area for which the Census Bureau collects and tabulates decennial census information Visible boundaries street road stream Shoreline Nonvisible boundaries county, city, neighborhood boundary property line 54 GIS TUTORIAL 1 - Basic Workbook INF385T(28437) – Spring 2013 – Lecture 5 54
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Census blocks 55 GIS TUTORIAL 1 - Basic Workbook
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Other TIGER layers 56 INF385T(28437) – Spring 2013 – Lecture 5
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U.S. Census Bureau data tables http://factfinder2.census.gov/ http://factfinder2.census.gov/ 57 INF385T(28437) – Spring 2013 – Lecture 5
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Summary File (SF1) tables 58 GIS TUTORIAL 1 - Basic Workbook
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Summary File (SF3) tables 59 INF385T(28437) – Spring 2013 – Lecture 5
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SF tables comparisons SF1 Population Age Sex Race Housing units FFH SF3 Income Educational attainment Citizenship Transportation Detailed housing 60 INF385T(28437) – Spring 2013 – Lecture 5
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Census summary Shapefiles downloaded from www.census.gov or www.esri.com Data tables downloaded from American Factfinder http://factfinder2.census.gov Data joins needed to join SF1 or SF3 to shapefiles INF385T(28437) – Spring 2013 – Lecture 5 61
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VECTOR DATA FORMATS Lecture 5 62 INF385T(28437) – Spring 2013 – Lecture 5
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ArcInfo coverages Created using ESRI’s ArcInfo software Older format (import/export as “.e00”) Set of files within a folder or directory called a workspace Files represent different types of topology or feature types 63 INF385T(28437) – Spring 2013 – Lecture 5
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Coverage attribute table Area and perimeter Coverage_ and Coverage_ID 64 INF385T(28437) – Spring 2013 – Lecture 5
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Shapefiles ArcView native format Minimum files .shp–stores feature geometry .shx–stores index of features .dbf–stores attribute data Additional files .prj–projection data .xml–metadata .sbn and.sbx–store additional indices 65 INF385T(28437) – Spring 2013 – Lecture 5
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CAD drawings CAD software Autodesk, AutoCAD (.dwg) Bentley, Microstation (.dgn,.dxf) Often used by engineering companies Architectural details, instructions to builders Roads, bridges, dams Better digitizing precision 66 INF385T(28437) – Spring 2013 – Lecture 5
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CAD drawings 67 INF385T(28437) – Spring 2013 – Lecture 5
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CAD layers 68 INF385T(28437) – Spring 2013 – Lecture 5
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Event files Data table that includes map coordinates, such as latitude and longitude or projected coordinates 69 INF385T(28437) – Spring 2013 – Lecture 5
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Event files 70 INF385T(28437) – Spring 2013 – Lecture 5
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Export event files 71 INF385T(28437) – Spring 2013 – Lecture 5 Creates point features
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RASTER DATA FORMATS Lecture 5 72 INF385T(28437) – Spring 2013 – Lecture 5
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Digital file formats TIFF (Tagged Image File Format) .tif file extension Very high quality images Commonly used in publishing Sizes are large because it is uncompressed GIF (Graphic Interchange Format): .gif as its file extension. Ideal for schematic drawings that have relatively large areas with solid color fill and few color variations. Small file sizes 73 INF385T(28437) – Spring 2013 – Lecture 5
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Digital file formats JPEG (Joint Photographic Experts Group): .jpg file extension. Most widely used format for photographs and other images that have a lot of color variations Uses file compression at the expense of picture detail, if you specify a lot of compression 74 INF385T(28437) – Spring 2013 – Lecture 5
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Summary Models of the Earth Map projections Coordinate systems GIS data sources Vector data formats Raster data formats 75 INF385T(28437) – Spring 2013 – Lecture 5
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