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A sunphotometer was also used to derive the aerosol optical thickness and ozone concentration.\\nSeawater samples were collected at the surface and maximum chlorophyll fluorescence using the CTD-rosette system. Surface seawater was also collected from the barge and a bucket. Particulate absorption, CDOM, pigment concentrations (HPLC) and particulate organic carbon and nitrogen content samples were collected at 24, 21 and 19 stations respectively. All water samples were stored frozen. The analyses were achieved in laboratories at Laval University and the University of Qu\\u00e9bec at Rimouski. Particulate absorption was measured following Rottgers & Gehnke (2012) method using a Perkin-Elmer lambda 850 spectrophotometer, CDOM was measured using a variable pathlength spectrophotometer (Ultrapath), pigment were analyzed following Zapata et al. (2000) method and POC-PON were analyzed using a CHNS/O elementary analyzer.\\nThe UVP enables identification and enumeration of zooplancton species and of sediment with size up to 200 \\u00b5m. The open source software provided with the instrument is dedicated to the study of big particles (>100 \\u00b5m) and study of zooplankton (mesozooplancton and micronecton). Pictures processing is achieved in a delayed mode.   The UVP was deployed systematically at each CTD cast but for leg1a where it was under repair.\\\", \\\"edition-date\\\": \\\"\\\", \\\"publisher\\\": \\\"\\\", \\\"title\\\": \\\"Optical properties and carbon fluxes of the Eastern Canadian Arctic Ocean\\\", \\\"version\\\": \\\"1.0\\\", \\\"language\\\": \\\"en\\\", \\\"URL\\\": \\\"https://catalogue.cioos.ca/dataset/ca-cioos_ccin-12076?local=en\\\"}]","fr":"[{\\\"type\\\": \\\"dataset\\\", \\\"id\\\": \\\"ca.cioos_ccin-12076\\\", \\\"author\\\": [{\\\"given\\\": \\\"Marcel\\\", \\\"family\\\": \\\"Babin\\\"}, {\\\"given\\\": \\\"Simon\\\", \\\"family\\\": \\\"B\\u00e9langer\\\"}, {\\\"given\\\": \\\"Joannie\\\", \\\"family\\\": \\\"Ferland\\\"}, {\\\"given\\\": \\\"Claudie\\\", \\\"family\\\": \\\"Marec\\\"}, {\\\"given\\\": \\\"Julien\\\", \\\"family\\\": \\\"Lalibert\\u00e9\\\"}, {\\\"given\\\": \\\"Zo\\u00e9\\\", \\\"family\\\": \\\"Amor\\u00e9na\\\"}], \\\"issued\\\": [{\\\"date-parts\\\": [\\\"2015\\\", \\\"02\\\", \\\"09\\\"]}], \\\"abstract\\\": \\\"Les propri\\u00e9t\\u00e9s optiques apparentes et inh\\u00e9rentes (AOP et IOPs), la mesure des stocks d'\\u00e9chantillons d'eau de mer et les profils de distribution des particules et de la faune \\u00e0 l'aide d'un profileur de vision sous-marine (UVP) ont \\u00e9t\\u00e9 \\u00e9tudi\\u00e9s du 8 juillet au 14 ao\\u00fbt (\\u00e9tape 1) principalement dans la mer du Labrador, la baie de Baffin et le d\\u00e9troit de Lancaster. 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En ce qui concerne la radiom\\u00e9trie au-dessus de l'eau, l'irradiance descendante incidente multispectrale (Ed0+ \\u00e0 15 longueurs d'onde) a \\u00e9t\\u00e9 mesur\\u00e9e en continu depuis le pont sup\\u00e9rieur \\u00e0 l'aide d'un irradiancem\\u00e8tre (biosph\\u00e9rique) mont\\u00e9 sur un m\\u00e2t t\\u00e9lescopique de 5 m. Un photom\\u00e8tre solaire a \\u00e9galement \\u00e9t\\u00e9 utilis\\u00e9 pour calculer l'\\u00e9paisseur optique de l'a\\u00e9rosol et la concentration d'ozone.\\nDes \\u00e9chantillons d'eau de mer ont \\u00e9t\\u00e9 collect\\u00e9s \\u00e0 la surface et \\u00e0 une fluorescence maximale de la chlorophylle \\u00e0 l'aide du syst\\u00e8me CTD-Rosette. L'eau de mer de surface a \\u00e9galement \\u00e9t\\u00e9 collect\\u00e9e \\u00e0 partir de la barge et d'un seau. 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(2000) et le POC-PON a \\u00e9t\\u00e9 analys\\u00e9 \\u00e0 l'aide d'un analyseur \\u00e9l\\u00e9mentaire CHNS/O.\\nL'UVP permet l'identification et le d\\u00e9nombrement des esp\\u00e8ces de zooplancton et des s\\u00e9diments dont la taille peut atteindre 200 \\u00b5m. Le logiciel open source fourni avec l'instrument est d\\u00e9di\\u00e9 \\u00e0 l'\\u00e9tude des grosses particules (>100 \\u00b5m) et \\u00e0 l'\\u00e9tude du zooplancton (m\\u00e9sozooplancton et micronecton). Le traitement des images s'effectue en mode diff\\u00e9r\\u00e9. 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It aims to advance scientific knowledge and understanding of these polar environments through collaborative research initiatives.","fr":"Amundsen Science est un programme de recherche canadien axé sur les régions arctiques et antarctiques. Il vise à faire progresser les connaissances scientifiques et la compréhension de ces environnements polaires grâce à des initiatives de recherche collaboratives."}},"license_title":"Creative Commons Attribution 4.0","num_resources":1,"resource-type":"dataset","bbox-east-long":"-55.38","bbox-north-lat":"81.22","bbox-south-lat":"53.92","bbox-west-long":"-149.0","creator_user_id":"fe6035ee-ed91-4ead-b5b2-4048232a22bb","temporal-extent":[{"end":"2014-09-25","begin":"2014-07-08"}],"vertical-extent":[{"max":"0","min":"0"}],"aggregation-info":[{"initiative-type":"","association-type":"crossReference","aggregate-dataset-name":{"en":"Polar Data Catalogue equivalent record","fr":"Enregistrement équivalent du Catalogue de données polaires"},"aggregate-dataset-identifier_code":"https://www.polardata.ca/pdcsearch/PDCSearchDOI.jsp?doi_id=12076"}],"maintainer_email":null,"maintenance-note":"Generated from https://cioos-siooc.github.io/metadata-entry-form#/en/amundsen/c8GqCtwH6sZnf3HtZhCgkOsmtoh1/ccin-12076","metadata_created":"2026-09-05T17:46:05.211009","notes_translated":{"en":"Apparent and inherent optical properties (AOPs and IOPs), stock measurement of seawater samples and particles and fauna distribution profiles with an Underwater Visio Profiler (UVP) were studied from July 8 to August 14 (Leg 1) mainly in the Labrador Sea, Baffin Bay and Lancaster Sound. Some measurements were made further North in the Nares Strait and the Kennedy Channel. As the UVP was integrated in the CTD/rosette system of the Amundsen, it was deployed through out the expedition until September 25th in Beaufort and Chuckchi Seas.\nFor the IOPs, 27 stations were sampled during Leg 1. IOPs profiles were measured using 2 optical packages, which include the following sensors: backscattering meters (from HobiLabs Hydroscat-6), fluorometers for colored dissolved organic matter absorption (CDOM) and chlorophyll. AOPs profiles were measured using a Compact-Optical Profiling System with 15 wavelengths (Biospherical). As for above-water radiometry, multispectral incident downwelling irradiance (Ed0+ at 15 wavelengths) was measured continuously from the top bridge using an irradiance meter (Biospherical) mounted on a 5-m telescoping mast. A sunphotometer was also used to derive the aerosol optical thickness and ozone concentration.\nSeawater samples were collected at the surface and maximum chlorophyll fluorescence using the CTD-rosette system. Surface seawater was also collected from the barge and a bucket. Particulate absorption, CDOM, pigment concentrations (HPLC) and particulate organic carbon and nitrogen content samples were collected at 24, 21 and 19 stations respectively. All water samples were stored frozen. The analyses were achieved in laboratories at Laval University and the University of Québec at Rimouski. Particulate absorption was measured following Rottgers & Gehnke (2012) method using a Perkin-Elmer lambda 850 spectrophotometer, CDOM was measured using a variable pathlength spectrophotometer (Ultrapath), pigment were analyzed following Zapata et al. (2000) method and POC-PON were analyzed using a CHNS/O elementary analyzer.\nThe UVP enables identification and enumeration of zooplancton species and of sediment with size up to 200 µm. The open source software provided with the instrument is dedicated to the study of big particles (>100 µm) and study of zooplankton (mesozooplancton and micronecton). Pictures processing is achieved in a delayed mode.   The UVP was deployed systematically at each CTD cast but for leg1a where it was under repair.","fr":"Les propriétés optiques apparentes et inhérentes (AOP et IOPs), la mesure des stocks d'échantillons d'eau de mer et les profils de distribution des particules et de la faune à l'aide d'un profileur de vision sous-marine (UVP) ont été étudiés du 8 juillet au 14 août (étape 1) principalement dans la mer du Labrador, la baie de Baffin et le détroit de Lancaster. Certaines mesures ont été effectuées plus au nord dans le détroit de Nares et le canal Kennedy. L'UVP étant intégré au système CTD/Rosette de l'Amundsen, il a été déployé tout au long de l'expédition jusqu'au 25 septembre dans les mers de Beaufort et de Chuckchi.\nPour les IOP, 27 stations ont été échantillonnées au cours de l'étape 1. Les profils IOPS ont été mesurés à l'aide de 2 boîtiers optiques, qui comprennent les capteurs suivants : des compteurs à rétrodiffusion (de HobiLabs Hydroscat-6), des fluoromètres pour l'absorption de matière organique dissoute colorée (CDOM) et la chlorophylle. Les profils AOP ont été mesurés à l'aide d'un système de profilage optique compact à 15 longueurs d'onde (biosphérique). En ce qui concerne la radiométrie au-dessus de l'eau, l'irradiance descendante incidente multispectrale (Ed0+ à 15 longueurs d'onde) a été mesurée en continu depuis le pont supérieur à l'aide d'un irradiancemètre (biosphérique) monté sur un mât télescopique de 5 m. Un photomètre solaire a également été utilisé pour calculer l'épaisseur optique de l'aérosol et la concentration d'ozone.\nDes échantillons d'eau de mer ont été collectés à la surface et à une fluorescence maximale de la chlorophylle à l'aide du système CTD-Rosette. L'eau de mer de surface a également été collectée à partir de la barge et d'un seau. Des échantillons d'absorption de particules, de CDOM, de concentrations de pigments (HPLC) et de teneur en carbone organique particulaire et en azote ont été collectés à 24, 21 et 19 stations respectivement. Tous les échantillons d'eau ont été conservés congelés. Les analyses ont été réalisées dans des laboratoires de l'Université Laval et de l'Université du Québec à Rimouski. L'absorption des particules a été mesurée selon la méthode de Rottgers & Gehnke (2012) à l'aide d'un spectrophotomètre Perkin-Elmer lambda 850, le CDOM a été mesuré à l'aide d'un spectrophotomètre à longueur de trajet variable (Ultrapath), les pigments ont été analysés selon la méthode de Zapata et al. (2000) et le POC-PON a été analysé à l'aide d'un analyseur élémentaire CHNS/O.\nL'UVP permet l'identification et le dénombrement des espèces de zooplancton et des sédiments dont la taille peut atteindre 200 µm. Le logiciel open source fourni avec l'instrument est dédié à l'étude des grosses particules (>100 µm) et à l'étude du zooplancton (mésozooplancton et micronecton). Le traitement des images s'effectue en mode différé. L'UVP a été déployé systématiquement sur chaque moulage CTD, sauf pour la phase 1a où il était en réparation."},"title_translated":{"en":"Optical properties and carbon fluxes of the Eastern Canadian Arctic Ocean","fr":"Propriétés optiques et flux de carbone de l'est de l'océan Arctique canadien"},"xml_location_url":"https://waf.forms.cioos.ca/metadata/amundsen/laval-university/ccin-12076.xml","metadata-language":"en","metadata_modified":"2026-09-05T17:46:05.211013","frequency-of-update":"asNeeded","dataset-reference-date":[{"type":"creation","value":"2014-07-08"},{"type":"publication","value":"2015-02-09"},{"type":"revision","value":"2015-02-09"}],"cited-responsible-party":[{"role":"principalInvestigator","individual-name":"Babin, Marcel","organisation-name":"","contact-info_email":"","contact-info_online-resource":""},{"role":"originator","individual-name":"Bélanger, 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<mri:abstract xsi:type=\"lan:PT_FreeText_PropertyType\">\n        <gco:CharacterString>Apparent and inherent optical properties (AOPs and IOPs), stock measurement of seawater samples and particles and fauna distribution profiles with an Underwater Visio Profiler (UVP) were studied from July 8 to August 14 (Leg 1) mainly in the Labrador Sea, Baffin Bay and Lancaster Sound. Some measurements were made further North in the Nares Strait and the Kennedy Channel. As the UVP was integrated in the CTD/rosette system of the Amundsen, it was deployed through out the expedition until September 25th in Beaufort and Chuckchi Seas.\r\nFor the IOPs, 27 stations were sampled during Leg 1. IOPs profiles were measured using 2 optical packages, which include the following sensors: backscattering meters (from HobiLabs Hydroscat-6), fluorometers for colored dissolved organic matter absorption (CDOM) and chlorophyll. AOPs profiles were measured using a Compact-Optical Profiling System with 15 wavelengths (Biospherical). As for above-water radiometry, multispectral incident downwelling irradiance (Ed0+ at 15 wavelengths) was measured continuously from the top bridge using an irradiance meter (Biospherical) mounted on a 5-m telescoping mast. A sunphotometer was also used to derive the aerosol optical thickness and ozone concentration.\r\nSeawater samples were collected at the surface and maximum chlorophyll fluorescence using the CTD-rosette system. Surface seawater was also collected from the barge and a bucket. Particulate absorption, CDOM, pigment concentrations (HPLC) and particulate organic carbon and nitrogen content samples were collected at 24, 21 and 19 stations respectively. All water samples were stored frozen. The analyses were achieved in laboratories at Laval University and the University of Québec at Rimouski. Particulate absorption was measured following Rottgers &amp; Gehnke (2012) method using a Perkin-Elmer lambda 850 spectrophotometer, CDOM was measured using a variable pathlength spectrophotometer (Ultrapath), pigment were analyzed following Zapata et al. (2000) method and POC-PON were analyzed using a CHNS/O elementary analyzer.\r\nThe UVP enables identification and enumeration of zooplancton species and of sediment with size up to 200 µm. The open source software provided with the instrument is dedicated to the study of big particles (&gt;100 µm) and study of zooplankton (mesozooplancton and micronecton). Pictures processing is achieved in a delayed mode.   The UVP was deployed systematically at each CTD cast but for leg1a where it was under repair.</gco:CharacterString>\n        <lan:PT_FreeText>\n          <lan:textGroup xlink:href=\"https://cioos.ca/translation_method\" xlink:role=\"translation\" xlink:title=\"text translated using the Amazon translate service / texte traduit à l&#39;aide du service de traduction Amazon\">\n            <lan:LocalisedCharacterString locale=\"#fr\">Les propriétés optiques apparentes et inhérentes (AOP et IOPs), la mesure des stocks d&#39;échantillons d&#39;eau de mer et les profils de distribution des particules et de la faune à l&#39;aide d&#39;un profileur de vision sous-marine (UVP) ont été étudiés du 8 juillet au 14 août (étape 1) principalement dans la mer du Labrador, la baie de Baffin et le détroit de Lancaster. Certaines mesures ont été effectuées plus au nord dans le détroit de Nares et le canal Kennedy. L&#39;UVP étant intégré au système CTD/Rosette de l&#39;Amundsen, il a été déployé tout au long de l&#39;expédition jusqu&#39;au 25 septembre dans les mers de Beaufort et de Chuckchi.\r\nPour les IOP, 27 stations ont été échantillonnées au cours de l&#39;étape 1. Les profils IOPS ont été mesurés à l&#39;aide de 2 boîtiers optiques, qui comprennent les capteurs suivants : des compteurs à rétrodiffusion (de HobiLabs Hydroscat-6), des fluoromètres pour l&#39;absorption de matière organique dissoute colorée (CDOM) et la chlorophylle. Les profils AOP ont été mesurés à l&#39;aide d&#39;un système de profilage optique compact à 15 longueurs d&#39;onde (biosphérique). En ce qui concerne la radiométrie au-dessus de l&#39;eau, l&#39;irradiance descendante incidente multispectrale (Ed0+ à 15 longueurs d&#39;onde) a été mesurée en continu depuis le pont supérieur à l&#39;aide d&#39;un irradiancemètre (biosphérique) monté sur un mât télescopique de 5 m. Un photomètre solaire a également été utilisé pour calculer l&#39;épaisseur optique de l&#39;aérosol et la concentration d&#39;ozone.\r\nDes échantillons d&#39;eau de mer ont été collectés à la surface et à une fluorescence maximale de la chlorophylle à l&#39;aide du système CTD-Rosette. L&#39;eau de mer de surface a également été collectée à partir de la barge et d&#39;un seau. Des échantillons d&#39;absorption de particules, de CDOM, de concentrations de pigments (HPLC) et de teneur en carbone organique particulaire et en azote ont été collectés à 24, 21 et 19 stations respectivement. Tous les échantillons d&#39;eau ont été conservés congelés. Les analyses ont été réalisées dans des laboratoires de l&#39;Université Laval et de l&#39;Université du Québec à Rimouski. L&#39;absorption des particules a été mesurée selon la méthode de Rottgers &amp; Gehnke (2012) à l&#39;aide d&#39;un spectrophotomètre Perkin-Elmer lambda 850, le CDOM a été mesuré à l&#39;aide d&#39;un spectrophotomètre à longueur de trajet variable (Ultrapath), les pigments ont été analysés selon la méthode de Zapata et al. (2000) et le POC-PON a été analysé à l&#39;aide d&#39;un analyseur élémentaire CHNS/O.\r\nL&#39;UVP permet l&#39;identification et le dénombrement des espèces de zooplancton et des sédiments dont la taille peut atteindre 200 µm. Le logiciel open source fourni avec l&#39;instrument est dédié à l&#39;étude des grosses particules (&gt;100 µm) et à l&#39;étude du zooplancton (mésozooplancton et micronecton). Le traitement des images s&#39;effectue en mode différé. L&#39;UVP a été déployé systématiquement sur chaque moulage CTD, sauf pour la phase 1a où il était en réparation.</lan:LocalisedCharacterString>\n          </lan:textGroup>\n        </lan:PT_FreeText>\n      </mri:abstract>\n      <mri:credit>\n        <gco:CharacterString></gco:CharacterString>\n      </mri:credit>\n      <mri:status>\n        <mcc:MD_ProgressCode codeList=\"http://standards.iso.org/iso/19115/resources/Codelists/cat/codelists.xml#MD_ProgressCode\" codeListValue=\"underDevelopment\"></mcc:MD_ProgressCode>\n      </mri:status>\n      <mri:topicCategory>\n        <mri:MD_TopicCategoryCode>oceans</mri:MD_TopicCategoryCode>\n      </mri:topicCategory>\n      <mri:extent>\n        <gex:EX_Extent>\n          <gex:geographicElement>\n            <gex:EX_GeographicBoundingBox>\n              <gex:extentTypeCode>\n                <gco:Boolean>true</gco:Boolean>\n              </gex:extentTypeCode>\n              <gex:westBoundLongitude>\n                <gco:Decimal>-149.0</gco:Decimal>\n              </gex:westBoundLongitude>\n              <gex:eastBoundLongitude>\n                <gco:Decimal>-55.38</gco:Decimal>\n              </gex:eastBoundLongitude>\n              <gex:southBoundLatitude>\n                <gco:Decimal>53.92</gco:Decimal>\n              </gex:southBoundLatitude>\n              <gex:northBoundLatitude>\n                <gco:Decimal>81.22</gco:Decimal>\n              </gex:northBoundLatitude>\n            </gex:EX_GeographicBoundingBox>\n          </gex:geographicElement>\n        </gex:EX_Extent>\n      </mri:extent>\n      <mri:extent>\n        <gex:EX_Extent>\n          <gex:geographicElement>\n            <gex:EX_GeographicDescription>\n              <gex:extentTypeCode>\n                <gco:Boolean>true</gco:Boolean>\n              </gex:extentTypeCode>\n              <gex:geographicIdentifier>\n                <mcc:MD_Identifier>\n                  <mcc:code>\n                    <gco:CharacterString></gco:CharacterString>\n                  </mcc:code>\n                  <mcc:codeSpace>\n                    <gco:CharacterString>ca.cioos</gco:CharacterString>\n                  </mcc:codeSpace>\n                  <mcc:version>\n                    <gco:CharacterString>1</gco:CharacterString>\n                  </mcc:version>\n                  <mcc:description>\n                    <gco:CharacterString>{&#39;en&#39;: &#39;Labrador Sea, Baffin Bay, Lancaster Sound, Nares Strait, Kennedy Channel, Beaufort Sea, and Chukchi Sea&#39;}</gco:CharacterString>\n                  </mcc:description>\n                </mcc:MD_Identifier>\n              </gex:geographicIdentifier>\n            </gex:EX_GeographicDescription>\n          </gex:geographicElement>\n        </gex:EX_Extent>\n      </mri:extent>\n      <mri:extent>\n        <gex:EX_Extent>\n          <gex:verticalElement>\n            <gex:EX_VerticalExtent>\n              <gex:minimumValue>\n                <gco:Real>0</gco:Real>\n              </gex:minimumValue>\n              <gex:maximumValue>\n                <gco:Real>0</gco:Real>\n              </gex:maximumValue>\n              <gex:verticalCRSId>\n                <mrs:MD_ReferenceSystem>\n                  <mrs:referenceSystemIdentifier>\n                    <mcc:MD_Identifier>\n                      <mcc:code>\n                        <gco:CharacterString>5829</gco:CharacterString>\n                      </mcc:code>\n                      <mcc:codeSpace>\n                        <gco:CharacterString>EPSG</gco:CharacterString>\n                      </mcc:codeSpace>\n                      <mcc:version>\n                        <gco:CharacterString>2012-08-10T00:00:00</gco:CharacterString>\n                      </mcc:version>\n                      <mcc:description>\n                        <gco:CharacterString>Instantaneous Water Level height - Height relative to instantaneous water level uncorrected for tide. Not specific to any location or epoch.</gco:CharacterString>\n                      </mcc:description>\n                    </mcc:MD_Identifier>\n                  </mrs:referenceSystemIdentifier>\n                  <mrs:referenceSystemType>\n                    <mrs:MD_ReferenceSystemTypeCode codeList=\"https://standards.iso.org/iso/19115/resources/Codelists/cat/codelists.xml#MD_ReferenceSystemTypeCode\" codeListValue=\"vertical\">vertical</mrs:MD_ReferenceSystemTypeCode>\n                  </mrs:referenceSystemType>\n                </mrs:MD_ReferenceSystem>\n              </gex:verticalCRSId>\n              <gex:verticalCRS xlink:href=\"http://www.epsg-registry.org/export.htm?gml=urn:ogc:def:crs:EPSG::5831\" xlink:title=\"instantaneous water level depth\" xlink:actuate=\"onRequest\" />\n            </gex:EX_VerticalExtent>\n          </gex:verticalElement>\n        </gex:EX_Extent>\n      </mri:extent>\n      <mri:extent>\n        <gex:EX_Extent>\n          <gex:temporalElement>\n   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