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<resTitle>Hydro_Enforced_DTM_2018</resTitle>
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<fgdcGeoform>remote-sensing image</fgdcGeoform>
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<idAbs>&lt;DIV STYLE="text-align:Left;"&gt;&lt;DIV&gt;&lt;DIV&gt;&lt;P&gt;&lt;SPAN&gt;Hydro-Flattened Bare Earth DTM. The dataset was created using the lidar bare earth points and 3D hydro breaklines to a resolution of 1 m (April 2018).Voids exist in the data due to data redaction conducted under the guidance of the United States Secret Service. All lidar data returns and collected data were removed from the dataset based on the redaction footprint shapefile generated in 2017.&lt;/SPAN&gt;&lt;/P&gt;&lt;/DIV&gt;&lt;/DIV&gt;&lt;/DIV&gt;</idAbs>
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<resTitle>ISO 19115 Topic Categories</resTitle>
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<keyword>elevation</keyword>
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<srcDesc>The hydro-breaklines were collected in 2D as vector line work, using a combination of classified lidar dataset, intensity images, shaded relief TIN and contours. The hydro features were collected to the following specifications: double line rivers and streams greater than 10’ in width, ponds or lakes greater than .5 acre, and islands greater than .25 acre. After the breaklines have been collected, vertex elevation values were assigned using a distance weighted distribution of the lidar points closest to each vertex (similar to draping the 2D linework to a surface modelled from the lidar points). The linework elevation values were further adjusted based on the following rules: 1) lake feature vertices were re-assigned (flattened) to the lowest draped vertex value, and 2) double stream bank line vertices were re-assigned based on the vertices of the closest adjusted double stream connector line. Fugro proprietary software was used to create profiles to ensure bank-to-bank flatness, monotonicity check and lake flatness.</srcDesc>
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