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            <gco:CharacterString>Attribute accuracy for habitat polygons has not been conducted. Field checks of all benthic signatures present in the photographs were conducted to resolve those benthic features that potentially could be confused with submersed rooted vegetation. The number and locations of site visits were based on judgment of the photointerpreter who led the field verification phase of the surface level sampling. In a second type of surface level work, a grid was randomly placed on a nautical chart to determine the nominal latitude and longitude of stations. These were sampled for species of submersed rooted vegetation and ancillary environmental information. The methodology was inappropriate for accuracy assessment of the remotely based habitat data for three  reasons.

1) Any plants within a quarter mile radius of the station's coordinates were sampled and indicated as positive in the field database. Rare occurrences of small clusters of plants would not be mapped from the photographs due to the minimum mapping unit.

2) Navigation to stations was accomplished with LORAN C, which was spatially much less accurate than was expected with the photographic approach. Reference data must be a more reliable source than the data to be evaluated.

3) Some nominal station locations were unexpectedly deep or unsafe to approach or sample and were arbitrarily moved to an adjacent more appropriate location. This could have biased the spatial sampling.</gco:CharacterString>
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            <gco:CharacterString>Horizontal positional accuracy has not been established for the data set. National Map Accuracy standards (at a compilation scale of 1:24,000) are assumed as the theoretical optimal accuracy of this data. Accuracy is limited by the accuracy and temporal coincidence of the basemap and the interpretation of the aquatic bed data from photographs. In the case of USGS 7.5' topographic maps, the cultural information is more contemporary (up to 10 or 15 years out of date) than the geographic information (up to 45 years out of date). NOAA shoreline and cultural data (based on 1988 and 1991 photography) are within six years of the aquatic bed photography. The dearth of cultural information throughout most of the study area resulted in a dependency on geographic features for local horizontal control of the photographic data. The aquatic bed photographs were more consistent with contemporary NOAA shoreline topographic map bases (from 1988 and 1991) photography and use of these map bases presumably increased overall accuracy of the vegetation map. Aerial  photography is registered by local horizontal control to basemaps in a zoom transfer scope. Reference features are readily identifiable and can be accurately positioned on the photograph and on the basemap. Cultural feature are preferred and geographic features are used if necessary. The basemaps are USGS 7.5' topographic series or NOAA shoreline topographic sheets.</gco:CharacterString>
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          <gmd:result gco:nilReason="missing" />
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            <gco:CharacterString>Vertical Positional Accuracy</gco:CharacterString>
          </gmd:nameOfMeasure>
          <gmd:evaluationMethodDescription>
            <gco:CharacterString>The SRV data carries no vertical attributes, and no assessment or measure of vertical accuracy was conducted.</gco:CharacterString>
          </gmd:evaluationMethodDescription>
          <gmd:result gco:nilReason="missing" />
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      <gmd:report>
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            <gco:CharacterString>Completeness Report</gco:CharacterString>
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          <gmd:evaluationMethodDescription>
            <gco:CharacterString>The classification scheme includes one class at the Class level and one at the Subclass 1 level within the SCHEME system. All SRV within the study area were delineated, unless flagged in the data set, to a depth of approximately 10 feet mean lower low water (MLLW), deeper than aquatic beds are known to grown in the study area. Limited parts of the study area were not successfully photographed and therefore data for those locations are omitted from the coverage. The photography provides a record of only a single time period so that ephemeral beds not present at the time of photography are omitted. This may be the case for some Zostera marina beds, for example, which can sprout from seed in the late spring and die due to heat stress and exposure in the summer. Zostera marina is a perennial grass which over winters as rhizomes within the substrate.</gco:CharacterString>
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      <gmd:report>
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            <gco:CharacterString>Conceptual Consistency</gco:CharacterString>
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          <gmd:evaluationMethodDescription>
            <gco:CharacterString>The classification scheme comprehensively includes all subtidal bottom classified for the presence or absence of submersed rooted vegetation. Void areas exceeding minimum mapping unit were mapped within vegetation polygons and are delineated and labeled. Overlay of the compiled and digitized polygons of vegetation included a few instances of overlap with dry land on the map base. This was particularly true for data compiled on 7.5' map bases due to the time differential between the photographic dates for the map bases (typically 1940s for shorelines and 1970s or 1980s for cultural features) and the aquatic bed photography (1985 to 1990). The shoreline moved in some cases. Logical consistency in terms of topology for vegetation polygons was confirmed in ARC/INFO and test plots of the digitized data at the compilation scale (1:24,000) were compared for consistency and similarity of cartographic style with the source maps and were edited if necessary.</gco:CharacterString>
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          <gmd:result gco:nilReason="missing" />
        </gmd:DQ_ConceptualConsistency>
      </gmd:report>
      <gmd:lineage>
        <gmd:LI_Lineage>
          <gmd:statement gco:nilReason="missing" />
          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>Acquisition of metric aerial photography: Conventional color aerial photography was collected in several missions between 1985 and 1990 following the protocols described in NOAA Technical Report NMFS 123. Both film diapositives and paper prints were used for the interpretation.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>1990-01-01T00:00:00</gco:DateTime>
              </gmd:dateTime>
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          </gmd:processStep>
          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>Compilation of photographic information: Aerial photos were interpreted and habitats delineated on acetate overlays affixed to the film. Field information was used to guide this mapping process. The interpreted photo delineations were then transferred to hard-copy base maps using a zoom-transfer scope to fit the polygons to a planimetric base.

Photointerpretation with a Wild AVIOPRET stereoscope. Photographs and data were compiled on a Bausch and Lomb stereo zoom transfer scope at a scale of 1:24,000 on USGS 7.5' topographic maps or on NOAA shoreline topographic sheets scaled to 1:24,000 (original scale 1:20,000). Data is a merge of several coverages dependent on map base, photo mission, and photographic scale.</gco:CharacterString>
              </gmd:description>
              <gmd:dateTime>
                <gco:DateTime>1990-01-01T00:00:00</gco:DateTime>
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          <gmd:processStep>
            <gmd:LI_ProcessStep>
              <gmd:description>
                <gco:CharacterString>Digitization of compiled photographic interpretations: 1:24,000 scale bases were supplied to CGIA by the NOAA/NMFS/SEFSC/Beaufort Lab. These were used to digitize the delineated areas of SRV. All digital files were later compiled into one digital GIS data set. Checkplots were created for review by the Beaufort Lab and any corrections made.</gco:CharacterString>
              </gmd:description>
            </gmd:LI_ProcessStep>
          </gmd:processStep>
          <gmd:processStep>
            <gmd:LI_ProcessStep>
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              <gmd:dateTime>
                <gco:DateTime>2015-01-01T00:00:00</gco:DateTime>
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          </gmd:processStep>
          <gmd:processStep>
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                <gco:CharacterString>Standardized common design elements, cleaned up field content, repaired geometry, and projected to NAD83.</gco:CharacterString>
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              <gmd:dateTime>
                <gco:DateTime>2025-08-01T00:00:00</gco:DateTime>
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                <gco:CharacterString>Source Contribution: Source photography for SAV interpretation (film diapositives)</gco:CharacterString>
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                        <gco:Date>1990-01-01</gco:Date>
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                        <gco:CharacterString>NOS Photogrammetry Branch</gco:CharacterString>
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