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        <gco:CharacterString>Wessex Archaeology was commissioned by Royal Haskoning DHV on behalf of Dudgeon Offshore Wind Limited (DOW) to conduct an archaeological assessment of geophysical data obtained over
the site of the Dudgeon Offshore Wind Farm and its associated export cable route. An archaeological interpretation and assessment of sidescan sonar, magnetometer and multibeam bathymetry data was undertaken. 

For the purpose of reporting, the study area was separated into the Offshore Wind Farm and the export Cable Route. The Dudgeon Offshore Wind Farm site is situated approximately 32km offshore of Cromer on the north Norfolk coast. The Offshore Wind Farm comprises 67 wind turbine locations and their associated Inter-array cables. A 500m corridor for the Inter-array Cables and a 50m radius buffer zone for each of the wind turbine locations were assessed. The export cable route will make landfall as Weybourne Hope, approximately 5km west of Sheringham; with a 500m corridor being assessed.</gco:CharacterString>
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                    <gco:CharacterString>Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services</gco:CharacterString>
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                        <gco:Date>2010-12-08T00:00:00</gco:Date>
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                <gco:CharacterString>Conformity with the Commission Regulation (EU) No 1089/2010 was either not relevant to this dataset or not a requirement of the Marine Data Exchange for the creation and submission of this dataset; therefore, conformity has not been assessed and cannot be declared</gco:CharacterString>
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            <gco:CharacterString>The sidescan sonar data were processed by WA using Coda Geosurvey software. This allowed the data to be replayed with various gain settings in order to optimise the quality of the images. The data were initially scanned to give an understanding of the geological nature of the area and were then interpreted for any objects of possible anthropogenic origin. This involves creating a database of anomalies within Coda by tagging individual features of possible archaeological potential, recording their positions and dimensions, and acquiring an image of each anomaly for future reference.
A mosaic of the sidescan sonar data is produced during the data processing to assess the quality of the sonar towfish positioning. This allows the position of anomalies to be checked between different survey lines and for the layback values to be further refined if necessary. The navigation information was contained within the data files themselves and errors on positioning are +/-5m. The magnetometer data were processed by WA using Geometrics MagPick software in order to identify any discrete magnetic contacts which could represent buried metallic debris or structures such as wrecks. The software enables both visualisation of individual lines of data and gridding of data to produce a magnetic anomaly map. Smoothed averages of the data were first calculated, and then subtracted from the raw data values in order to reduce the effect of natural variations in the magnetic field such as changes in geology or water depth. The 0.2m cell size of the multibeam bathymetry data was too small for the quality of the data with some data holes apparent and collection artefacts very apparent. WA gridded the provided data with a coarser resolution of 1m and made digital terrain maps using IVS Fledermaus software. These data were examined for evidence of anomalies identified in the sidescan data. The initial interpretation of the geophysical data sets is conducted independently of each other. This inevitably leads to the possibility of any one object being the cause of numerous anomalies in different datasets and apparently overstating the number of
archaeological features in the area. To address this fact, the anomalies were grouped together. This allows one ID number to be assigned to a single object for which there may be, for example, a bathymetric anomaly and multiple sidescan sonar anomalies. Once all the geophysical anomalies have been grouped, a discrimination flag is added to the record in order to discriminate against those which are not thought to be of an archaeological concern. The sidescan, magnetic and bathymetry anomalies were grouped together where they correlate. UKHO records that fall within the target review areas were included and grouped where appropriate. This produced the final gazetteer of features. These features are numbered with a WA ID which takes the form of a 70,000 number series. Anomalies that were identified during the previous phases of work (WA, 2009a, and b) were included and grouped where appropriate and have retained their original 7000 numbers. Due to the
better quality of the most recent datasets, those anomalies identified during both the current and previous phases of work have had their locations updated.  It must be noted that the current data set is of a higher quality than those used during previous reports (WA, 2009a and b). The small 35m range of the sidescan sonar dataset allows for higher resolution and therefore identification of smaller anomalies that may not have been identified during the previous phase. The recent magnetometer dataset as been acquired at UXO standard and as such at a much higher specification compared to
previous surveys and as such an increased number of anomalies have been identified during this assessment.</gco:CharacterString>
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        <gco:CharacterString>ABP Marine Environmental Research</gco:CharacterString>
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                    <gco:Date>2022-12-12</gco:Date>
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            <gmx:Anchor xlink:href="https://apps.epsg.org/api/v1/ProjectedCoordRefSystem/32631">WGS 84 / UTM zone 31N</gmx:Anchor>
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