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      <gmd:resourceConstraints>
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                        <gmd:CI_OnlineResource>
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Relative accuracy of the swaths compared to overlapping and adjacent swaths was verified through the use of Delta-Z (DZ) orthos created in LASTools software. Profiles of elevated planar features, such as roofs, were used to verify horizontal alignment between overlapping swaths.

The NovAtel software was utilized for GPS and inertial processing, Data were processed to an initial LAS format using the Leica Lidar Survey Studio software. 

Algorithms in TerraScan was used to create the initial ground surface.

All lidar data was peer-reviewed. QAQC also included creating void polygons for use during review.  All necessary edits were applied to the dataset.  LASTools was used to update LAS header information, including all projection and coordinate reference system information.  The final lidar data is in LAS format 1.4 and point data record format 6.

Data were processed in NAD83 (PA11) horizontal and vertical datum.  The National Oceanic and Atmospheric Administration (NOAA) received files in laz format.
	
The files contained lidar elevation and intensity measurements. With the exception of Niihau, data was delivered in UTM Zone 3 coordinates and ellipsoid elevations in meters.

Horizontal Datum-NAD83 (PA11) epoch: 2010.0
Projection-UTM Zone 3 North
Horizontal Units-meters
Vertical Datum-NAD83 (PA11) Ellipsoid height
Vertical Units-meters


 The final classification scheme for all data delivered to NOAA is as follows:
1-Unclassified
2-Ground
7-Low Noise
9-Topo Water Surface
18-High Noise
40-Bathymetric Point
41-Bathymetric Water Surface
42-Synthetic Derived Water Surface
43-Submerged Object
44-International Hydrographic Organization (IHO) S-57 Object
64-Submerged Aquatic Vegetation
65-Bathymetric Bottom Temporal Changes</gco:CharacterString>
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              <gmd:dateTime>
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          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>The lidar data is referenced to the NAD83 (PA11) ellipsoid.  The GEOID12B model does not exist over the AOI.  The lidar data in ellipsoid heights was used to create the final topobathymetric DEMs in ellipsoid heights.

Lidar data were used to generate a raster in geotiff format with 1 meter pixel resolution for the entire area.  The raster was then clipped to the tile grid and named according to project specifications to result in tiled topobathymetric DEMs.

Bathy void polygons represent bathymetric areas with no bathymetric bottom returns and accompany the DEMs. Void polygon creation is described in the final project report and the void polygon metadata.

A confidence layer has been created and provided to NOAA as part of the deliverables. Except where there are not enough lidar data points in a pixel to calculate a standard deviation value, the confidence layer is a raster product in geotiff format with 1 meter square pixels.  The confidence layer provides a standard deviation value for every pixel by calculating the standard deviation of all ground and/or submerged topography lidar points that are located within a single pixel.  The confidence layer pixels align to the pixels in the topobathy DEMs.  The confidence layer can be displayed by unique values or classified into desired bins/ranges for analysis over larger areas.</gco:CharacterString>
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