Sun & hill
topographic methods
Yesterday in the Great Smokies
Webcam
archive
UKy Geography Colloquium, 2025
Boyd Shearer
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Senior Lecturer, Department of Geography
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Online Digital Mapping program π
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outrageGIS mapping trail maps π
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Contact π
D Rumsey Map Collection
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Eduard Imhof, 1895-1986 π
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Carte de France, 1750-1815 π
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Tiled on a Google Map π
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Hans Conrad Gyger, 1599-1674 π
USGS Topographic maps
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7.5 minute quadrangles are gold standard.
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1880sβcurrent π
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USGS Topo View π― π
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Let's map forest trails.
First axiom: You must be present. Maps live in
the areas they show.
Second axiom: Places are
interconnected.
Lidar
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Lidar detection and ranging
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users lasers to sample the earth's surface
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and create a dense point cloud of elevations.
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KyFromAbove π
Height model
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Lidar captures above ground features.
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DSM: Digital Surface Model.
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DEM: Digital Elevation Model.
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height = DSM - DEM
First use of height model visualizing floods
2022 floods
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Identify informal infrastructure prone to flooding.
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Notably, private bridges.
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Relative elevation model (REM) for height above river.
A tree canopy model
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Use NAIP NDVI to identify trees.
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Extract heights from DSM.
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trees = (NDVI > x) & (height > y)
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National Agriculture Imagery Program (NAIP)
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Normalized Difference Vegetation Index (NDVI)
Caveats
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Temporal resolutions don't match.
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NAIP's profound vertical displacement.
Change: multitemporal analysis
Two statewide point clouds
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Simple math comparing DSMs.
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change = DSMP2 - DSMP1
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but trickier symbology.
Opportunities
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Fuse NDVI with DSM change
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to find loss and gain of tree canopy.
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loss = (NDVIP1 > x) & (heightP2-P1 < y)
Accurate?
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First axiom: get into the field.
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But, what about the historical observations?
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Google Maps Street View? π
π
Third axiom: Places change.
(And if change
is
incompatible with humans?)