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GIS georeferencing map projections coordinate systems

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This document provides a detailed overview of geographic information systems (GIS), focusing on georeferencing, geographic coordinate systems (GCS), map projections, and projected coordinate systems (PCS). The lecture notes cover key concepts and practical applications. It discusses systems for locating features on Earth and various types of maps.

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1. Introduction to Georeferencing ​ Definition: Georeferencing refers to the process of associating data with a specific location on Earth using coordinate systems. ​ Purpose: Enables GIS to represent features accurately on a map. Key Properties of Georeferencing Systems 1.​ Unique...

1. Introduction to Georeferencing ​ Definition: Georeferencing refers to the process of associating data with a specific location on Earth using coordinate systems. ​ Purpose: Enables GIS to represent features accurately on a map. Key Properties of Georeferencing Systems 1.​ Uniqueness: Locations must be uniquely identifiable (e.g., distinguishing Springfield, MO, from Springfield, UK). 2.​ Persistence: Locations remain consistent over time. 3.​ Spatial Resolution: Specifies level of detail (e.g., "Norman" is more precise than "Oklahoma"). 4.​ Metric vs. Non-Metric: ○​ Metric: Uses coordinate systems to calculate distances mathematically (e.g., lat/long). ○​ Non-Metric: Uses relative locations (e.g., "next to the river"). 2. Geographic Coordinate System (GCS) ​ Description: Uses latitude and longitude lines to specify locations. ​ Components: ○​ Latitude (Parallels): Measures north-south position. ​ Ranges from 0° at the equator to ±90° at the poles. ○​ Longitude (Meridians): Measures east-west position. ​ Ranges from 0° at the Prime Meridian (Greenwich, England) to ±180°. ​ Units: Angular degrees, minutes, and seconds (or decimal degrees). ○​ Example: Norman, OK = 35°13'N, 97°26'W. Terms to Remember ​ Meridian: A line of constant longitude. ​ Parallel: A line of constant latitude. ​ Unprojected Nature of GCS: Cannot compute accurate areas or distances without projection. 3. Map Projections ​ Purpose: Converts Earth’s 3D surface into a 2D map. ​ Challenges: Introduces distortions in: ○​ Area: Size of features. ○​ Shape: Geometric appearance. ○​ Distance: Space between points. ○​ Direction: Angles or bearings. Projection Properties 1.​ Equal-Area (Equivalent): Preserves area but distorts shape. 2.​ Conformal (Orthomorphic): Preserves shape but distorts area. 3.​ Equidistant: Preserves distances (only in specific areas). 4.​ True-Direction (Azimuthal): Preserves angles/directions. 5.​ Compromise: Balances distortion among properties. Projection Factors 1.​ Developable Surfaces: Shapes onto which the Earth is projected. ○​ Cylindrical: Gridlines form rectangles (e.g., Mercator). ○​ Conical: Gridlines curve (e.g., Albers Equal Area). ○​ Planar: Gridlines radiate from a central point (e.g., Azimuthal). 2.​ Aspect: Orientation of the developable surface. ○​ Normal: Aligned with the poles. ○​ Transverse: Aligned with the equator. ○​ Oblique: At an angle. 3.​ Viewpoint: Light source for projection. ○​ Gnomonic: From the Earth's center. ○​ Stereographic: From the far side of the globe. ○​ Orthographic: From infinity. 4.​ Case: Intersection of the developable surface with Earth. ○​ Tangent: Touches at one line or point. ○​ Secant: Cuts through the Earth. 4. Common Map Projections 1.​ Albers Equal Area: ○​ Type: Conic. ○​ Properties: Preserves area; distorts shape, distance, and direction. ○​ Uses: Regional/national maps. 2.​ Lambert Conformal Conic: ○​ Type: Conic. ○​ Properties: Preserves shape and direction; distorts area. ○​ Uses: Navigation, State Plane Coordinate System. 3.​ Mercator: ○​ Type: Cylindrical. ○​ Properties: Preserves direction and shape; distorts area at high latitudes. ○​ Uses: Navigation, world maps. 4.​ Azimuthal Equidistant: ○​ Type: Planar. ○​ Properties: Preserves distances and directions from a central point. ○​ Uses: Polar maps, air/sea navigation. 5. Projected Coordinate Systems (PCS) ​ Definition: A grid superimposed on a map projection to specify locations in a plane. ​ Components: ○​ Ellipsoid: A mathematical model of Earth’s shape (e.g., GRS80, WGS84). ○​ Datum: Links the ellipsoid to specific Earth locations (e.g., NAD83). ○​ Projection: Converts the 3D Earth into 2D coordinates. Common PCSs 1.​ Universal Transverse Mercator (UTM): ○​ Divides the globe into 60 zones, each 6° wide. ○​ Uses meters for coordinates (e.g., easting and northing). ○​ Popular for GPS mapping. 2.​ State Plane Coordinate System (SPCS): ○​ Divides states into smaller zones to minimize distortion. ○​ Uses different projections (e.g., Lambert for wide zones, Mercator for tall zones). 6. Practical Applications ​ GCS vs. PCS: ○​ GCS: Based on lat/long; unprojected; suitable for global contexts. ○​ PCS: Projected; allows accurate distance, area, and direction measurements. ​ Choosing the Right Projection: ○​ Depends on the purpose of the map: ​ Preserve area for population density studies. ​ Preserve distance for transportation routes. ​ Preserve direction for navigation.

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