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2014/07/16 Council Agenda Packet
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2014/07/16 Council Agenda Packet
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Council Agenda Packet
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7/16/2014
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APPENDIX C: LIDAR DISCLAIMER <br />The following excerpt has been extracted from the metadata for the Puget Sound LIDAR Consortium 2000 <br />dataset13: <br />Considerable care has been taken to ensure that these data are as accurate as possible. We <br />believe most of the data is adequate for determination of flood hazards, for geologic mapping, <br />for hydrologic modeling, for determination of slope angles, for modeling of radio -wave <br />transmission, and similar uses with a level of detail appropriate to a horizontal scale of <br />1:12,000 (1 inch = 1,000 feet) or smaller and vertical accuracy on the order of a foot. Locally, <br />the data is of considerably poorer quality. <br />In the bare earth DEMs [Digital Elevation Model] where there are few survey points (i.e. bare - <br />earth surfaces in heavy timber, where there are few ground reflections), TINing [Triangular <br />Irregular Network] the points produces large triangular facets where the surface has <br />significant curvature. Similar, though finer, textures are evident where vegetation reflections <br />are incompletely filtered. Elevations are likely to be less accurate in these areas. <br />LiDAR data values for water surfaces are not valid elevation values. LiDAR surveying <br />produces few survey points on water. Mirror-like surfaces fail to scatter the laser beam and <br />unless the beam is perpendicular to the surface, no light is reflected back to the detector. Or <br />intense reflections may lead to negative blunders, points that are too low. Interpolation <br />between the nearest on -land points and sparse water points produces large triangular facets <br />that may not accurately reflect the water -surface elevation. Where the water surface is <br />surveyed adequately, adjacent swaths may be flown at different tide stages, producing <br />swath -parallel cliffs. Ideally, LIDAR topography would be clipped to eliminate all open -water <br />areas, but at present this is very labor-intensive. <br />Users should carefully determine the place -to -place accuracy and fitness of these data for <br />your particular purposes. For many purposes a site- and use -specific field survey will be <br />necessary. <br />The accuracy specification in the contract between the Puget Sound LIDAR Consortium and <br />TerraPoint is based on a required Root Mean Square Error (RMSE) 'Bare Earth' vertical <br />accuracy of 30 cm for flat areas in the complete data set. This is the required result if all data <br />points in flat areas were evaluated. Because only a small sample of points is evaluated, the <br />required RMSE for the sample set is adjusted downward per the following equation from the <br />FEMA LIDAR specification (adjusted from the 15 cm RMSE in the FEMA specification to 30 <br />cm to accommodate the dense vegetation cover in the Pacific Northwest). <br />The Seattle and Bremerton LIDAR are part of the PSLC 2000 project. The Tacoma LiDAR is part of the <br />PSLC 2004 project. <br />t3 Full metadata is available on the PSLC website: http://pugetsoundlidar.ess.washington.edullidardata/metadata.html <br />L-27 <br />Appendix L: Climate Change Background <br />
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