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                            <gmd:CI_OnLineFunctionCode codeList="https://data.noaa.gov/resources/iso19139/schema/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode" codeListValue="information">information</gmd:CI_OnLineFunctionCode>
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      <gmd:resourceConstraints>
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                      <gmd:onlineResource>
                        <gmd:CI_OnlineResource>
                          <gmd:linkage>
                            <gmd:URL>https://www.fisheries.noaa.gov/inportserve/waf/noaa/nos/ngs/dmp/pdf/77189.pdf</gmd:URL>
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                            <gmd:CI_OnLineFunctionCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode" codeListValue="information">information</gmd:CI_OnLineFunctionCode>
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        <gco:CharacterString>The NOAA Maine Topbathymetric Lidar data includes all lidar returns. An automated grounding classification algorithm was used to determine bare earth and submerged topography point classification. The automated grounding was followed with manual editing. Classes 2 (ground), 40 (submerged topography), and 43 (submerged object) were used to create the final DEMs. The full workflow used for this project are documented in the NOAA Maine Topobathymetric Lidar final report.</gco:CharacterString>
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                <gmd:URL>https://coast.noaa.gov/dataviewer/#/lidar/search/where:ID=10423</gmd:URL>
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                <gco:CharacterString>WWW:LINK-1.0-http--link</gco:CharacterString>
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            <gco:CharacterString>Horizontal - Lidar horizontal accuracy is a function of Global Navigation Satellite System (GNSS) derived positional error, flying altitude, and INS derived attitude error. The obtained RMSEr value is multiplied by a conversion factor of 1.7308 to yield the horizontal component of the National Standards for Spatial Data Accuracy (NSSDA) reporting standard where a theoretical point will fall within the obtained radius 95 percent of the time (ACCr).

Vertical - Absolute accuracy was assessed using Non-Vegetated Vertical Accuracy (NVA) survey methods. Survey check points were evenly distributed as feasible throughout the project area. NVA compares known ground check point data that were withheld from the calibration and post-processing of the lidar point cloud to the triangulated surface generated by the ground classified lidar point cloud. NVA is a measure of the accuracy of lidar point data in open areas with level slope (less than 20 degrees) where the lidar system has a high probability of measuring the ground surface.

Non-Vegetated Vertical Accuracy (NVA),  Vegetated Vertical Accuracy (VVA) and submerged topography accuracy were evaluated at the 95% confidence interval (1.96*RMSE).</gco:CharacterString>
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            <gco:CharacterString>Horizontal Positional Accuracy</gco:CharacterString>
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          <gmd:evaluationMethodDescription>
            <gco:CharacterString>Block01_01:
At a flight altitude of 400 m, with an IMU error of 0.002 decimal degrees and a GNSS positional error of 0.005 m:

Leica Chiroptera: RMSEr = 0.025 m, ACCr = 0.040 m (95%).
Leica Hawkeye: RMSEr = 0.025 m, ACCr = 0.040 m (95%).

Block01_02:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:

Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.038 m, ACCr = 0.070 m (95%).

Block02_01:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:
Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.038 m, ACCr = 0.070 m (95%).

Block02_02:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:
Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.062 m, ACCr = 0.11 m (95%).

Block02_03:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:
Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.062 m, ACCr = 0.11 m (95%).

Block03_01:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:
Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.038 m, ACCr = 0.070 m (95%).

Block03_02:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.023 m:
Leica Chiroptera: RMSEr = 0.044 m, ACCr = 0.080 m (95%).
Leica Hawkeye: RMSEr = 0.131 m, ACCr = 0.23 m (95%).

Block04_01:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:
Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.038 m, ACCr = 0.070 m (95%).

Block04_02:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:
Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.038 m, ACCr = 0.070 m (95%).

Block04_03:
At a flight altitude of 400 m, with an IMU error of 0.003 decimal degrees and a GNSS positional error of 0.008 m:
Leica Chiroptera: RMSEr = 0.038 m, ACCr = 0.070 m (95%).
Leica Hawkeye: RMSEr = 0.038 m, ACCr = 0.070 m (95%).</gco:CharacterString>
          </gmd:evaluationMethodDescription>
          <gmd:result gco:nilReason="missing" />
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            <gco:CharacterString>Vertical Positional Accuracy</gco:CharacterString>
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          <gmd:evaluationMethodDescription>
            <gco:CharacterString>Block01_01 -  NVA tested 0.069 m using 5 ground check points based on RMSEz (0.035 m) x 1.9600.  Submerged topography accuracy tested 0.114 m using 114 submerged check points, based on RMSEz (0.058 m) x 1.9600.  

Block01_02 - NVA tested 0.069 m using 7 ground check points based on RMSEz (0.035 m) x 1.9600.  Submerged topography accuracy tested 0.169 m  using 90 submerged check points, based on RMSEz (0.086 m) x 1.9600.

Block02_01 - NVA tested 0.057 m using 6 ground check points based on RMSEz (0.029 m) x 1.9600.  VVA tested 0.109 m using 5 landclass points .  

Block02_02 - NVA tested 0.041 m using 9 ground check points based on RMSEz (0.021 m) x 1.9600.  VVA tested 0.196 m using 8 landclass points.

Block02_03 - NVA tested 0.032 m using 6 ground check points based on RMSEz (0.020 m) x 1.9600.  VVA tested 0.101 m vertical accuracy at the 95th percentile against the ground classified point cloud using 3 landclass points based on RMSEz (0.016 m) x 1.9600.

Block03_01 - NVA tested 0.040 m using 15 ground check points , based on RMSEz (0.020 m) x 1.9600.  Submerged topography accuracy tested 0.141 m using 160 submerged check points based on RMSEz (0.072 m) x 1.9600.

Block03_02 - NVA tested 0.069 m using 9 ground check points based on RMSEz (0.035 m) x 1.9600. Submerged topography accuracy tested 0.119 m using 223 submerged check points based on RMSEz (0.060 m) x 1.9600.

Block04_01 -  NVA tested 0.053 m using 8 ground check points based on RMSEz (0.027 m) x 1.9600. Submerged topography accuracy tested 0.137 m using 145 submerged check points based on RMSEz (0.070 m) x 1.9600. 

Block04_02 - NVA tested 0.059 m using 11 ground check points based on RMSEz (0.030 m) x 1.9600.  Submerged topography accuracy tested 0.103 m using 62 submerged check points based on RMSEz (0.053 m) x 1.9600.

Block04_03 - NVA tested 0.017 m using 4 ground check points based on RMSEz (0.009 m) x 1.9600.  Submerged topography accuracy tested 0.128 m using 83 submerged check points based on RMSEz (0.065 m) x 1.9600.</gco:CharacterString>
          </gmd:evaluationMethodDescription>
          <gmd:result gco:nilReason="missing" />
        </gmd:DQ_AbsoluteExternalPositionalAccuracy>
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            <gco:CharacterString>Comparability</gco:CharacterString>
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          <gmd:evaluationMethodDescription>
            <gco:CharacterString>Submerged topography checkpoints usually occurred in depths up to 1m.</gco:CharacterString>
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          <gmd:result gco:nilReason="missing" />
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            <gco:CharacterString>Completeness Report</gco:CharacterString>
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          <gmd:evaluationMethodDescription>
            <gco:CharacterString>The horizontal RMSEr value for the Leica Chiroptera shallow green and NIR sensor data.  The RMSEr value for the Leica Hawkeye deep green sensor data.</gco:CharacterString>
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          <gmd:result gco:nilReason="missing" />
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      <gmd:lineage>
        <gmd:LI_Lineage>
          <gmd:statement gco:nilReason="missing" />
          <gmd:processStep>
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              <gmd:description>
                <gco:CharacterString>Data for the NOAA Maine Topbathymetric Lidar Delivery was acquired by NV5 Geospatial (NV5) using Leica Chiroptera Hawkeye 4X and Leica Chiroptera Hawkeye 5 topobathymetric lidar systems. All derived LAS data is referenced to: 

				Horizontal Datum-NAD83(2011) epoch: 2010.00
				Projection-UTM Zone 19N
				Horizontal Units-meters
				Vertical Datum-GRS80 Ellipsoid
				Vertical Units-meters

NOAA provided NV5 Geospatial with a project boundary for the NOAA Maine Topobathymetric Lidar project. Using a 100 meter buffered boundary, NV5 created an airborne lidar acquisition plan. The collected lidar data were immediately processed in the field by NV5 to a level that will allow QA\QC measures to determine if the sensor is functioning properly and assess the coverage of submerged topography. An initial SBET was created using Waypoint Inertial Explorer 8.90, and the raw data were extracted into geo-referenced LAS files using Lidar Survey Studio 3.0 with pre-calculated scanner misalignment angles determined through a boresight protocol. These files were inspected for errors and then passed through an automated workflow, producing rasters to develop an initial assessment of bathymetric coverage. NV5 reviewed all acquired flight lines to ensure complete coverage and positional accuracy of the laser points. These rasters were also used to create an initial product in Quick Look Coverage Maps. These Quick Look files are not fully processed data or final products but provide rapid assessment of approximate coverage and depth penetration.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>2023-10-06T00:00:00</gco:DateTime>
              </gmd:dateTime>
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                <gmd:CI_ResponsibleParty>
                  <gmd:organisationName>
                    <gco:CharacterString>National Geodetic Survey</gco:CharacterString>
                  </gmd:organisationName>
                  <gmd:role>
                    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#gmd:CI_RoleCode" codeListValue="processor">processor</gmd:CI_RoleCode>
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          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>For Block 01_01, Block 01_02, Block 02_01, and Block 02_02,NV5 resolved kinematic corrections for aircraft position data using aircraft GNSS and Applanix's proprietary PP-RTX solution. When PP-RTX was not used NV5 conducted static Global Navigation Satellite System (GNSS) ground surveys (1 Hz recording frequency) using base stations over known monument locations during flights. After the airborne survey, static GPS data were triangulated with nearby Continuously Operating Reference Stations (CORS) using the Online Positioning User Service (OPUS) for precise positioning. Multiple independent sessions over the same base station were performed to confirm antenna height measurements and to refine position accuracy.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>2025-03-07T00:00:00</gco:DateTime>
              </gmd:dateTime>
              <gmd:processor>
                <gmd:CI_ResponsibleParty>
                  <gmd:organisationName>
                    <gco:CharacterString>National Geodetic Survey</gco:CharacterString>
                  </gmd:organisationName>
                  <gmd:role>
                    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#gmd:CI_RoleCode" codeListValue="processor">processor</gmd:CI_RoleCode>
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                </gmd:CI_ResponsibleParty>
              </gmd:processor>
            </gmd:LI_ProcessStep>
          </gmd:processStep>
          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>For Block 02_03, Block 03_01, Block 03_02, Block 04_01, Block 04_02 and Block 04_03, NV5 resolved kinematic corrections for the aircraft Global Navigation Satellite System (GNSS) data using static GPS data from Continuously Operating Reference Stations (CORS) utilizing the Online Positioning User Service (OPUS) for precise positioning. This data was used to correct the continuous on board measurements of the aircraft position recorded throughout the flight. When GNSS was not utilized, kinematic corrections for aircraft position data were corrected using aircraft GNSS and Novatel's proprietary PPP-AR solution.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>2025-03-07T00:00:00</gco:DateTime>
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                    <gco:CharacterString>National Geodetic Survey</gco:CharacterString>
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              </gmd:processor>
            </gmd:LI_ProcessStep>
          </gmd:processStep>
          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>This data was used to correct the continuous on board measurements of the aircraft position recorded throughout the flight. A final smoothed best estimate trajectory (SBET) was developed that blends post-processed aircraft position with attitude data. Using the SBETs, sensor head position and attitude were then calculated throughout the survey. Trimble Business Center v.3.90, Blue Marble Geographic Calculator 2019, and PosPac MMS 8.3 SP3 were used for these processes.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>2025-03-07T00:00:00</gco:DateTime>
              </gmd:dateTime>
              <gmd:processor>
                <gmd:CI_ResponsibleParty>
                  <gmd:organisationName>
                    <gco:CharacterString>National Geodetic Survey</gco:CharacterString>
                  </gmd:organisationName>
                  <gmd:role>
                    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#gmd:CI_RoleCode" codeListValue="processor">processor</gmd:CI_RoleCode>
                  </gmd:role>
                </gmd:CI_ResponsibleParty>
              </gmd:processor>
            </gmd:LI_ProcessStep>
          </gmd:processStep>
          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>Following the final SBET creation, NV5 used Leica Lidar Survey Studio (LSS) to calculate laser point positioning by associating SBET positions to each laser point return time, scan angle, and intensity. Leica LSS was used to derive a synthetic water surface to create a water surface model. Light travels at different speeds in air versus water and its direction of travel or angle is changed or refracted when entering the water column. The refraction tool corrects for this difference by adjusting the depth (distance traveled) and horizontal positioning (change of angle/direction) of the lidar data. All lidar data below water surface models were classified as water column to correct for refraction. Using raster-based QC methods, the output data is verified to ensure the refraction tool functioned properly.

Once all data was refracted by flight line, the data was exported to LAS 1.4 format and combined into 500 m x 500 m tiles. Data were then further calibrated using TerraMatch. NV5 used custom algorithms in TerraScan to classify the initial ground/submerged topography surface points.  Relative accuracy of overlapping swaths was compared and verified through the use Delta-Z (DZ) orthos created using NV5's Las Product Creator. Absolute vertical accuracy of the calibrated data was assessed using ground survey data and complete coverage was again verified.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>2023-10-06T00:00:00</gco:DateTime>
              </gmd:dateTime>
              <gmd:processor>
                <gmd:CI_ResponsibleParty>
                  <gmd:organisationName>
                    <gco:CharacterString>National Geodetic Survey</gco:CharacterString>
                  </gmd:organisationName>
                  <gmd:role>
                    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#gmd:CI_RoleCode" codeListValue="processor">processor</gmd:CI_RoleCode>
                  </gmd:role>
                </gmd:CI_ResponsibleParty>
              </gmd:processor>
            </gmd:LI_ProcessStep>
          </gmd:processStep>
          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>Post automated classification, NV5 then performed manual editing to review all classification and improve the final topobathymetric surface. NV5's LasMonkey was used to update LAS header information, including all projection and coordinate reference system information. The final lidar data are in LAS format 1.4 and point data record format 6.

The classification scheme delivered from the contractor is as follows:

1   - Unclassified
1W  - Withheld - edge clip 
1OW - Overlap Withheld - unrefracted green data from Chiroptera sensor
2   - Ground
7W  - Withheld -low noise
18W - Withheld - high noise
40  - Bathymetric bottom or submerged topography
41  - Water surface
42S - Synthetic- Chiroptera synthetic water surface
43  - Submerged feature
45  - Water column
64  - Submerged Aquatic Vegetation (SAV)
65O - Overlap bathy bottom - temporally different from a separate lift
71  - Unclassified associated with areas of overlap bathy bottom/temporal bathymetric differences
72  - Ground associated with areas of overlap bathy bottom/temporal bathymetric differences
81  - Water surface associated with areas of overlap bathy bottom/temporal bathymetric differences
82S - Synthetic - Chiroptera synthetic water surface associated with areas of overlap bathy bottom/temporal bathymetric differences
85  - Water column associated with areas of overlap bathy bottom/temporal bathymetric differences.

The channel bits are mapped as the following:
0 - Chiroptera green shallow laser
1 - Chiroptera/Hawkeye synthetic water surface
2 - Hawkeye green deep laser
3 - Chiroptera NIR

The user byte is mapped as the following:
10 - Chiroptera green shallow
11 - Chiroptera green shallow 4X
12 - Chiroptera green shallow synthetic
20 - Hawkeye green deep
21 - Hawkeye green deep 4X
22 - Hawkeye green deep synthetic
30 - Chiroptera NIR</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>2023-10-06T00:00:00</gco:DateTime>
              </gmd:dateTime>
              <gmd:processor>
                <gmd:CI_ResponsibleParty>
                  <gmd:organisationName>
                    <gco:CharacterString>National Geodetic Survey</gco:CharacterString>
                  </gmd:organisationName>
                  <gmd:role>
                    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#gmd:CI_RoleCode" codeListValue="processor">processor</gmd:CI_RoleCode>
                  </gmd:role>
                </gmd:CI_ResponsibleParty>
              </gmd:processor>
            </gmd:LI_ProcessStep>
          </gmd:processStep>
          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>The NOAA Office for Coastal Management (OCM) received files in laz format. The files contain lidar elevation and intensity measurements of the Maine (ME2201) blocks. The LiDAR data were in NAD83(2011) UTM Zone 19N coordinates and ellipsoid elevations in meters.

OCM performed the following processing on the data for Digital Coast storage and provisioning purposes: 1. Converted from UTM Zone 19 to geographic coordinates 2. Sorted by gps time and 3. reclassified point data. The final classification scheme is as follows. 1 - Unclassified, 2 - Ground, 7 - Low Noise, 22 - Temporal Exclusion, 40 - Bathymetric Point, 41 - Water Surface, 42 - Derived Water Surface, 43 - Submerged Object, 45 - Water Column, 64 - Submerged Vegetation and 65 - Submerged Temporal Exclusion.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>2025-08-29T00:00:00</gco:DateTime>
              </gmd:dateTime>
              <gmd:processor>
                <gmd:CI_ResponsibleParty>
                  <gmd:organisationName>
                    <gco:CharacterString>NOAA Office for Coastal Management</gco:CharacterString>
                  </gmd:organisationName>
                  <gmd:contactInfo>
                    <gmd:CI_Contact>
                      <gmd:phone>
                        <gmd:CI_Telephone>
                          <gmd:voice>
                            <gco:CharacterString>(843) 740-1202</gco:CharacterString>
                          </gmd:voice>
                        </gmd:CI_Telephone>
                      </gmd:phone>
                      <gmd:address>
                        <gmd:CI_Address>
                          <gmd:electronicMailAddress>
                            <gco:CharacterString>coastal.info@noaa.gov</gco:CharacterString>
                          </gmd:electronicMailAddress>
                        </gmd:CI_Address>
                      </gmd:address>
                    </gmd:CI_Contact>
                  </gmd:contactInfo>
                  <gmd:role>
                    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#gmd:CI_RoleCode" codeListValue="processor">processor</gmd:CI_RoleCode>
                  </gmd:role>
                </gmd:CI_ResponsibleParty>
              </gmd:processor>
            </gmd:LI_ProcessStep>
          </gmd:processStep>
          <gmd:source>
            <gmd:LI_Source>
              <gmd:sourceCitation>
                <gmd:CI_Citation>
                  <gmd:title>
                    <gco:CharacterString>Acquisition and Processing</gco:CharacterString>
                  </gmd:title>
                  <gmd:date gco:nilReason="missing" />
                  <gmd:citedResponsibleParty>
                    <gmd:CI_ResponsibleParty>
                      <gmd:organisationName>
                        <gco:CharacterString>NV5</gco:CharacterString>
                      </gmd:organisationName>
                      <gmd:role>
                        <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#gmd:CI_RoleCode" codeListValue="originator">originator</gmd:CI_RoleCode>
                      </gmd:role>
                    </gmd:CI_ResponsibleParty>
                  </gmd:citedResponsibleParty>
                </gmd:CI_Citation>
              </gmd:sourceCitation>
            </gmd:LI_Source>
          </gmd:source>
        </gmd:LI_Lineage>
      </gmd:lineage>
    </gmd:DQ_DataQuality>
  </gmd:dataQualityInfo>
</gmi:MI_Metadata>