Figure 10b (animation)

1:80K source generalized by RDP (left) and QTM (right)

click on top figures to re-animate, bottom figures for metadata

Nantucket MA 80K data RDP v. QTM gen.

Nantucket MA 80K data @ 1:250K

View Companion Figure 10a

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METADATA:

DATA: 1:80,000 NOAA/NOS digital nautical charts, vector coordinates in latitude and longitude

SOURCE: Coastline Extractor -- http://crusty.er.usgs.gov/coast/getcoast.html

EXTENT: 70¤ 14' W - 69¤ 58' W (W-E); 41¤ 14' N - 41¤ 23' N (S-N)

WIDTH: 22.67 km; HEIGHT: 17.06 km; AREA: 119.9 km2

LENGTH: 125.0 km; POINTS: 867; AVG SEG LEN: 0.14 km

PROJECTION: None for QTM generalization; plat carré (cosine) for RDP generalization and displayed maps.

INSETS: The smaller maps are drawn to the scale at which the QTM generalization is intended to be displayed. The scale you see depends on monitor resolution (images were produced at 75 DPI).

REMARKS: Data digitized from NOS charts at 1:80,000, possibly with insets digitized from charts as large as 1:10,000, conditioning unknown. It is possible that that the area around Nantucket town harbor was digitized from an inset. The 1:80K scale implies a resolution between 50 and 100 m (assuming a map resolution of 0.5 mm). As the average line segment length in the dataset is 200 m, this is not an unreasonable formulation.

In generalizing the data, RDP (Ramer-Douglas-Peucker algorithm) tolerances (100, 205, 490 m) were chosen to yield equal numbers of points as did the corresponding three levels of default non-hierarchical QTM (quaternary triangular mesh) generalization (levels 16, 15, 14 -- representing 150, 300 and 600 m ground resolution respectively).

No special treatment of local sinuosity was applied in these experiments. The sinuosity statistic gives the path-to-trendline ratio, averaged across the set of selected points (on a scale of 1 - 7). Note that the sinuosity of RDP solutions is consistently higher than that of QTM solutions; this is indicative of the "critical point" bias of RDP.

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