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Any conclusions drawn from the analysis of this information are not the responsibility of NOAA, the Office for Coastal Management or its partners</gco:CharacterString>
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                Qualitative value:0.05 meters RMSEz at 95 percent Confidence Interval., Test that produced the value:  The FVA was tested using 851 independent ground control points (GCPs) located in open terrain. The GCPs were distributed throughout the project area. Elevations from the unclassified LiDAR surface were measured for the x,y location of each check point. Elevations interpolated from the LiDAR surface were then compared to the elevation values of the surveyed control. The Root-Mean-Square (RMSE) was computed to be 0.03 m (0.09 ft.). Using withheld ground checkpoints, vertical accuracy has been tested to meet 0.05 m (0.17 ft.) FVA at 95 Percent confidence level using RMSE(z) x 1.9600 as defined by the National Standards for Spatial Data Accuracy (NSSDA); assessed and reported using National Digital Elevation Program (NDEP)/ASRPS Guidelines.</gco:CharacterString>
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               <gmd:result gco:nilReason="missing"/>
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                     <gmd:dateTime>
                        <gco:DateTime>2014-02-19T00:00:00</gco:DateTime>
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               <gmd:processStep>
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                        <gco:CharacterString>Hydro-Flattening.
        The bare-earth DEMs were created by triangulating all ground classified points and inserting 3-D breaklines by utilizing Terra-Solid’s TerraScan and TerraModeler software. Any ground points within one meter of the breaklines were reclassified to “ignored-ground” (ASPRS code: 10) before triangulation. The highest-hit DEMs were generated from “ground” and “default” classified points. In instances where “water” classified points had the highest elevation value, the water surface elevation from the bare-earth raster were used.</gco:CharacterString>
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                     <gmd:dateTime>
                        <gco:DateTime>2014-02-19T00:00:00</gco:DateTime>
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               <gmd:processStep>
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                        <gco:CharacterString>LiDAR Data Processing.  
				Flight lines and data were reviewed to ensure complete coverage of the study area and positional accuracy of the laser points.  Laser point return coordinates were computed using ALS Post Processor software and IPAS Pro GPS/INS software, based on independent data from the LiDAR system, IMU, and aircraft.  The raw LiDAR file was assembled into flight lines per return with each point having an associated x, y, and z coordinate.  Visual inspection of swath to swath laser point consistencies within the study area were used to perform manual refinements of system alignment.  Custom algorithms were designed to evaluate points between adjacent flight lines.  Automated system alignment was computed based upon randomly selected swath to swath accuracy measurements that consider elevation, slope, and intensities.  Specifically, refinement in the combination of system pitch, roll and yaw offset parameters optimize internal consistency.  Noise (e.g., pits and birds) was filtered using ALS post-processing software,  based on known elevation ranges and included the removal of any cycle slips.  Using TerraScan and MicroStation, ground classifications utilized custom settings appropriate to the study area.  The corrected and filtered return points were compared to the RTK ground survey points collected to verify the vertical and horizontal accuracies.  Points were output as laser points, TINed and GRIDed surfaces.</gco:CharacterString>
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                        <gco:DateTime>2014-02-19T00:00:00</gco:DateTime>
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               <gmd:processStep>
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                        <gco:CharacterString>NOAA Office for Coastal Management received the DEMs in imagine format with img and ige files. Data were converted to GeoTiff format with deflate compression using gdal_translate. Vertical georeferencing was also added.</gco:CharacterString>
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