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Introduction to GIS David R. Maidment
Center for Research in Water Resources University of Texas at Austin
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Presentation Outline Using GIS to connect hydrology and meteorology
Representation of spatial objects in GIS Terrain analysis using Digital Elevation Models Geodesy and map projections
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Hydrologic Cycle: Connecting the Land Surface with the Atmosphere
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Connecting Hydrology and Meteorology
Two Spatial Scales Drainage basin scale for consideration of severe storms and flood (Nexrad radar precipation as input, flood runoff as output) Regional or global scale for consideration of climate change (Global climate models as input, time series of river flows as output)
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Regional flood analysis in Houston
Study region
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Nexrad Rainfall for Storm of Oct 1994
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Discharge in Buffalo Bayou at Katy October, 1994 storm
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Calibrated Flow with HEC-HMS
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Global Runoff (mm/yr) According to NCAR’s CCM3.2 Global Climate Model (GCM)
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GTOPO30 - 30” Digital Elevation Model of the Earth
Source:
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Drainage in North America
Source:
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Drainage Basins of North America
Source:
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Streamflow Hydrographs for Large Basins
Runoff Input from Climate Model Streamflow Output at River Mouth Amazon River MacKenzie River Yangtze River Congo River
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A Fundamental Dilemma Land Surface Hydrology has:
drainage patterns organized by rivers and watersheds which are spatially discrete analysis in Cartesian coordinates (x,y,z) Atmospheric Science has: circulation patterns which are spatially continuous over the earth analysis in Geographic coordinates (f, l, z) GIS can be used to connect these two spatial frameworks
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Presentation Outline Using GIS to connect hydrology and meteorology
Representation of spatial objects in GIS Terrain analysis using Digital Elevation Models Geodesy and map projections
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Discrete and Continuous Space
Discrete Space: Vector GIS Continuous Space: Raster GIS
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Geospatial Database: a set of compatible data layers or themes
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Spatial Data: Vector format
Vector data are defined spatially: (x1,y1) Point - a pair of x and y coordinates vertex Line - a sequence of points Node DRM Polygon - a closed set of lines
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Feature Attribute Table
Fields Records
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Relational Linkages Descriptive Attributes Spatial Attributes
Water Right Locations Descriptive Attributes
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Locations on the Stream Network
Digital Stream Network Connects Control Point Locations
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Watersheds defined using a Digital Elevation Model
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Spatial Data: Raster format
Cell size Number of rows NODATA cell (X,Y) Number of Columns Definition of a Grid in GIS
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Points as Cells
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Line as a Sequence of Cells
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Polygon as a Zone of Cells
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Raster-Vector Data Model
Real World
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Presentation Outline Using GIS to connect hydrology and meteorology
Representation of spatial objects in GIS Terrain analysis using Digital Elevation Models Geodesy and map projections
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Study Region in West Austin
Hog Pen Ck 4 km 4 km
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Watershed Delineation by Hand Digitizing
Watershed divide Drainage direction Outlet
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30 Meter Mesh Standard for 1:24,000 Scale Maps
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DEM Elevations 720 720 Contours 740 720 700 680 740 720 700 680
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DEM Elevations Contours 700 680
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Eight Direction Pour Point Model
32 16 8 64 4 128 1 2
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Direction of Steepest Descent
1 1 67 56 49 53 44 37 58 55 22 67 56 49 53 44 37 58 55 22 Slope:
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Flow Direction Grid 2 4 8 1 16 128
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Austin West 30 Meter DEM Elevations in meters ftp://ftp. tnris. state
Austin West 30 Meter DEM Elevations in meters ftp://ftp.tnris.state.tx.us/tnris/demA.html
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Flow Direction Grid 32 16 8 64 4 128 1 2
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Grid Network
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Flow Accumulation Grid
3 2 3 2 2 2 11 1 1 11 1 15 1 15 2 5 2 5 24 1 1 24 Link to Grid calculator
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Flow Accumulation > 5 Cell Threshold
3 2 11 1 15 24 5
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Stream Network for 5 cell Threshold Drainage Area
3 2 2 1 11 1 15 2 5 1 24
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Streams with 200 cell Threshold (>18 hectares or 13
Streams with 200 cell Threshold (>18 hectares or 13.5 acres drainage area)
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Watershed Outlet
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Watershed Draining to This Outlet
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Watershed and Drainage Paths Delineated from 30m DEM
Automated method is more consistent than hand delineation
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DEM Data Sources 30m DEMs from 1:24,000 scale maps (urban watersheds)
3" (100m) DEMs from 1:250,000 scale maps (rural watersheds) 15" (500m) DEM for the US resampled from 3” DEM (large drainage basins) 30" (1km) DEM of the earth (GTOPO30)
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Presentation Outline Using GIS to connect hydrology and meteorology
Representation of spatial objects in GIS Terrain analysis using Digital Elevation Models Geodesy and map projections
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Shape of the Earth It is actually a spheroid, slightly larger in radius at the equator than at the poles We think of the earth as a sphere
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Geographic Coordinates (f, l, z)
Latitude (f) and Longitude (l) defined using an ellipsoid, an ellipse rotated about an axis Elevation (z) defined using geoid, a surface of constant gravitational potential Earth datums define standard values of the ellipsoid and geoid
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Ellipse Z b O a X F1 F2 P An ellipse is defined by:
Focal length = Distance (F1, P, F2) is constant for all points on ellipse When = 0, ellipse = circle Z b O a X F1 F2 For the earth: Major axis, a = 6378 km Minor axis, b = 6357 km Flattening ratio, f = (a-b)/a ~ 1/300 P
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Ellipsoid or Spheroid Rotate an ellipse around an axis
Z b O a a Y X Rotational axis
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Representations of the Earth
Mean Sea Level is a surface of constant gravitational potential called the Geoid Earth surface Ellipsoid Sea surface Geoid
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Definition of Elevation
Elevation Z P z = zp • z = 0 Land Surface Mean Sea level = Geoid Elevation is measured from the Geoid
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Coordinate System A planar coordinate system is defined by a pair
of orthogonal (x,y) axes drawn through an origin Y X Origin (xo,yo) (fo,lo)
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Earth to Globe to Map Map Projection: Map Scale: Scale Factor
Representative Fraction Globe distance Earth distance = Scale Factor Map distance Globe distance = (e.g. 1:24,000) (e.g )
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Conic Projections (Albers Equal Area, Lambert Conformal Conic)
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Cylindrical Projections (Universal Transverse Mercator)
Oblique
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Azimuthal (Lambert Azimuthal Equal Area)
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Presentation Summary Using GIS to connect hydrology and meteorology
Representation of spatial objects in GIS Terrain analysis using Digital Elevation Models Geodesy and map projections
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