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                  <gmd:CI_Citation>
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               <gmd:keyword>
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         <gmd:resourceConstraints>
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         <gmd:supplementalInformation>
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               <gmd:version>
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         <gmd:distributionFormat>
            <gmd:MD_Format>
               <gmd:name>
                  <gmx:Anchor xlink:href="http://vocab.nerc.ac.uk/collection/M01/current/TXT/">Text or Plaintext</gmx:Anchor>
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               <gmd:version>
                  <gco:CharacterString>1</gco:CharacterString>
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         <gmd:distributor/>
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               <gmd:onLine>
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                        <gmd:URL>https://cloud.emodnet-ingestion.eu/index.php/s/ZFcv057v553nJ0t</gmd:URL>
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                     <gmd:protocol>
                        <gco:CharacterString>WWW:DOWNLOAD-1.0-http--download</gco:CharacterString>
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               <gmd:onLine>
                  <gmd:CI_OnlineResource>
                     <gmd:linkage>
                        <gmd:URL/>
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                     <gmd:protocol>
                        <gco:CharacterString>WWW:LINK-1.0-http--link</gco:CharacterString>
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                        <gmd:CI_OnLineFunctionCode codeList="http://standards.iso.org/iso/19139/resources/gmxCodelists.xml#CI_OnLineFunctionCode"
                                                   codeListValue="information"/>
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         <gmd:transferOptions/>
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  <gmd:dataQualityInfo>
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                  <gmd:MD_ScopeCode codeList="http://standards.iso.org/iso/19139/resources/gmxCodelists.xml#MD_ScopeCode"
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         <gmd:report>
            <gmd:DQ_DomainConsistency xsi:type="gmd:DQ_DomainConsistency_Type">
               <gmd:result>
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                     <gmd:specification>
                        <gmd:CI_Citation>
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                              <gco:CharacterString>COMMISSION REGULATION (EC) No 1205/2008 of 3 December 2008 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards metadata</gco:CharacterString>
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                                 <gmd:date>
                                    <gco:Date>2010-12-08</gco:Date>
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                                 <gmd:dateType>
                                    <gmd:CI_DateTypeCode codeList="http://standards.iso.org/iso/19139/resources/gmxCodelists.xml#CI_DateTypeCode"
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                              </gmd:CI_Date>
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                        </gmd:CI_Citation>
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                     <gmd:explanation>
                        <gco:CharacterString>See the referenced specification</gco:CharacterString>
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                     <gmd:pass>
                        <gco:Boolean>false</gco:Boolean>
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         <gmd:report>
            <gmd:DQ_DomainConsistency xsi:type="gmd:DQ_DomainConsistency_Type">
               <gmd:result>
                  <gmd:DQ_ConformanceResult xsi:type="gmd:DQ_ConformanceResult_Type">
                     <gmd:specification>
                        <gmd:CI_Citation>
                           <gmd:title>
                              <gco:CharacterString>Corrigendum to INSPIRE Metadata Regulation published in the Official Journal of the European Union, L 328, page 83</gco:CharacterString>
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                                 <gmd:date>
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                                 <gmd:dateType>
                                    <gmd:CI_DateTypeCode codeList="http://standards.iso.org/iso/19139/resources/gmxCodelists.xml#CI_DateTypeCode"
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                        <gco:CharacterString>See the referenced specification</gco:CharacterString>
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                     <gmd:pass>
                        <gco:Boolean>false</gco:Boolean>
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         <gmd:report>
            <gmd:DQ_DomainConsistency xsi:type="gmd:DQ_DomainConsistency_Type">
               <gmd:result>
                  <gmd:DQ_ConformanceResult xsi:type="gmd:DQ_ConformanceResult_Type">
                     <gmd:specification>
                        <gmd:CI_Citation>
                           <gmd:title>
                              <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>
                           </gmd:title>
                           <gmd:date>
                              <gmd:CI_Date>
                                 <gmd:date>
                                    <gco:Date>2010-12-08</gco:Date>
                                 </gmd:date>
                                 <gmd:dateType>
                                    <gmd:CI_DateTypeCode codeList="http://standards.iso.org/iso/19139/resources/gmxCodelists.xml#CI_DateTypeCode"
                                                         codeListValue="publication"/>
                                 </gmd:dateType>
                              </gmd:CI_Date>
                           </gmd:date>
                        </gmd:CI_Citation>
                     </gmd:specification>
                     <gmd:explanation>
                        <gco:CharacterString>See the referenced specification</gco:CharacterString>
                     </gmd:explanation>
                     <gmd:pass>
                        <gco:Boolean>false</gco:Boolean>
                     </gmd:pass>
                  </gmd:DQ_ConformanceResult>
               </gmd:result>
            </gmd:DQ_DomainConsistency>
         </gmd:report>
         <gmd:lineage>
            <gmd:LI_Lineage>
               <gmd:statement>
                  <gco:CharacterString>On the basis of the CTD stations, five transects cutting across the main bathymetrical and hydrographical structures of the study area were defined (Fig. 1) and interpolated for salinity, temperature, and fluorescence, respectively (Fig. 2). Transects 1-4 cut across the entire study area, starting in CSW, moving through DB, and ending in GSW. Transect 5 is located mainly in GSW, with only one station in DB (Fig. 1). All transects were characterized by relatively warm water (2.2 °C) in the upper water column (0-50 m) (Fig. 2a, d, g, j, m). In CSW, the intermediate water body (50-250 m) consisted of relatively cold water (-1.4 °C), which stretched out eastwards into the upper part of the intermediate water body in DB. In GSW, the intermediate water body was relatively warm (2.3 °C). The deeper part of the water body (250–500 m) was relatively warm in all three areas (2.1 °C) with a gradual increase in temperature from CSW toward GSW. On all transects, the salinity ranged from 30.5 to 34.5, increasing with depth. The salinity was in general lowest in the surface waters (0–50 m) of the CSW and highest at depth (300–500 m) in the GSW (Fig. 2b, e, h, k, n), the latter as a result of the inflow of warm Atlantic water. At any particular depth, salinity always increased toward east. Fluorescent material was only found in the upper 50 m of the water column with slightly higher values in CSW and GSW(0.9) than inDB(0.6) (Fig. 2c, f, i, l, o). St. 1 located on the shallow St. Hellefiskebanke (GSW), which is renowned for its primary production, had the highest fluorescence levels recorded in the study area. However, if st. 1 is excluded, there were significantly higher levels of fluorescent material in CSW than in GSW (p[0.0001, t test).|Between September 7 and September 22, 2009, a total of
45 stations were sampled from the research vessel R/V
Bjarni Sæmundsson (Marine Research Institute, Reykjavik,
Iceland). Sampling was carried out during full 24-h cycles,
every 4–6 h. The survey was initiated at Sisimiut
(Southwest Greenland) and covered a route of 1,485 nautical
miles (nmi). The order of the station numbers corresponds to the chronological sequence of the survey.
The survey route transects the main bathymetric and
hydrographical features described above. For the ease of
presentation, the study area was subdivided into three
areas: Canadian Shelf Waters (CSWs), DB, and Greenland
Shelf Waters (GSWs). Stations shallower than 700 m are
assigned to CSW on the Canadian side and to GSW on the
Greenland side, whereas stations deeper than 700 m are
defined as DB. One exception to this rule is
station st. 37, which is assigned to DB even though it is
shallower than 700 m. This was done because it is located
in the central part of the study area far off the regular
shelves and surrounded by much deeper water. It presumably
represents a very localized peak in DB, which has not
before been captured in bathymetry data collections
(Jakobsson et al. 2012). At all 45 stations, vertical profiles of temperature, salinity and fluorescence were obtained from the surface down to
500 m using a SBE 9 plus CTD (SeaBird Electronics)
equipped with a Seapoint chlorophyll fluorometer (Seapoint
Sensors Inc). Due to an unfortunate loss of samples, the
fluorescence readings could not be calibrated to the study
area and are therefore only used as a proxy for the relative
differences in Chlorophyll-a concentration between stations.</gco:CharacterString>
               </gmd:statement>
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         </gmd:lineage>
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  </gmd:dataQualityInfo>
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