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On Some Fundamental Geographical Concepts 176B Lecture 3
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Nystuen, J. D. (1963) “Identification of some fundamental spatial concepts” Search for a common geographical terminology to eliminate redundancy Basics: Distance, pattern, relative position, site and accessibility Advantages of abstract models and assumptions, e.g. isotropic surface
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The mosque floor
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Geographic primitives G = g (x, y, z, s, A, t) [x, y, z] = f( d Geography also highly dependent upon model
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UCSB Lat: 34.4087 Lon: -119.8447
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Projection, datum etc. for a 7.5 min quad
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GIS basic geometric functions A GIS package must be able to move between –map projections –coordinate systems –datums –Ellipsoids A GIS must be able to GEORECTIFY Not always a simple task!
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Orthorectification
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Georegistration: Control
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Georectification
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Conflation
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Address matching 2123 South Main St. Anywhere CA 93901 4,312,205mN 623,864mE 15N
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Geographic information fundamentals 1. Volume 2. Dimensionality 3. Continuity
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Volume 1 meter pixel 24 bit depth (8 bit R, 8 bit G, 8 bit B) California 3 rd largest State A=158,706 square miles A= 411,046,653,039 square meters N=9.865x10^10 bytes 98 gigabyte image
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Volume Issues: Tiles and Pyramids
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Dimensionality Simple geographic features can be used to build more complex ones. Areas are made up of lines which are made up of points represented by their coordinates. Areas = {Lines} = {Points}
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Areas are lines are points are coordinates
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Continuity Attributes of the earth fall into different spatial “behaviors” over space and time Many phenomena are best treated as continuous fields –E.g. air temperature, atmospheric pressure, population density Others have distinct spatial extent or edges –E.g. census tracts, buildings, roads
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Field vs. Feature (object)
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Fields are often rasters
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Air Photos Discontinuous irregular rasters: resampling 1929
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Features are often vectors
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Properties of Features Size Distribution/density Shape Scale Orientation
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Size: Resolution and Extent 10cm, 25cm, 50cm, 1m
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Resels: Non-uniform Support
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Data structure conversion
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Distribution
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Geographical Clustering
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Clusters on points/networks
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Shape
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Shape vs. Support
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Shape measures/analysis
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Scale: RF vs. Detail Santa Barbara
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Scaling behavior
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Orientation: Objects & Frame
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Tobler’s First Law of Geography “Everything is related to everything else but near things are more related than distant things” (Tobler, 1970) Variation of (x 1 – x 0 ) 2 Spatial autocorrelation Violates assumptions of statistics
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Geographical relations Among features –Contains/overlaps/intersects –Contiguity/Adjacency –Proximity –Trajectory Within fields –Neighborhood relation –Pattern –Process
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Vector polygon overlay O =
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Raster overlay 0 1 & =
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Buffering
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Pattern
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Pattern (Fourier) Analysis
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Contiguity http://www.clearproject.net/chapter10fig5.JPG (Clear Lake, Iowa)
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Semivariogram
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Most important, process… G = g (x, y, z, s, A, t) t0t0 t1t1 t2t2 t3t3
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Strands
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Time-Space dynamics
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Dynamics 19301950197019801990 FROM TO
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Geography The study of the earth and its features and of the distribution of life on the earth, including human life and the effects of human activity.
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