{"help":"https://catalogue.cioos.ca/api/3/action/help_show?name=package_show","success":true,"result":{"id":"65ebed19-3c9b-4347-8938-8158ff324b71","ecv":["surface_currents"],"eov":["subSurfaceCurrents","subSurfaceSalinity","subSurfaceTemperature","surfaceCurrents","other"],"url":null,"name":"ca-cioos_348ca0d9-6de9-4bd8-9dbd-ccf89f9810491","tags":[],"type":"dataset","notes":"Le Programme de surveillance hors plateau de la zone Atlantique (AZOMP) recueille et analyse les observations océanographiques physiques, chimiques et biologiques du talus continental et des bassins profonds de l'Atlantique Nord-Ouest, dans le but global de surveiller la variabilité du climat océanique et du plancton affectant les écosystèmes au large du Canada atlantique et les systèmes climatiques à l'échelle régionale et mondiale. \n\nLes mesures annuelles dans la mer du Labrador ont débuté en 1990 dans le cadre de l'expérience mondiale sur la circulation océanique (WOCE) et ont évolué pour devenir un effort de surveillance régional multidisciplinaire intégré au Programme mondial d'enquêtes hydrographiques à base de navires océaniques (GO-SHIP).\n\nLe programme d'échantillonnage d'AZOMP au large du Canada atlantique et de la mer du Labrador comprend l'échantillonnage annuel de la ligne Atlantic Repeat 7-West (AR7W), une ligne de 880 km traversant la mer du Labrador depuis la côte du Labrador jusqu'à la côte groenlandaise et une extension de la ligne Halifax, ainsi que des stations en eau profonde au-dessus du Scotian Slope and Rise situées à l'extrémité de la ligne Halifax de l'AZMP. 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La convection transfère également les gaz atmosphériques de la surface vers des profondeurs intermédiaires, ce qui réduit le taux d'augmentation du dioxyde de carbone dans l'atmosphère mais augmente l'acidité de l'océan.","state":"active","title":"Données chronologiques amarrées du Programme de surveillance hors plateau de la zone Atlantique (AZOMP) de la région des Maritimes","author":null,"extras":[{"key":"access_constraints","value":""},{"key":"contact-email","value":"Marc.Ringuette@dfo-mpo.gc.ca"},{"key":"encoding","value":"utf8"},{"key":"guid","value":"ca.cioos_348ca0d9-6de9-4bd8-9dbd-ccf89f981049"},{"key":"h_job_id","value":"dd85bc4c-b884-4922-8c5a-915d0f2edaca"},{"key":"h_object_id","value":"b5fcd4ba-b138-4c5b-9345-32adadcb8b1a"},{"key":"h_source_id","value":"f0527ee7-d937-4f5a-97f2-4687fd2c7d1a"},{"key":"h_source_title","value":"CIOOS Atlantic"},{"key":"h_source_url","value":"https://catalogue.cioosatlantic.ca"},{"key":"harvest_object_id","value":"b5fcd4ba-b138-4c5b-9345-32adadcb8b1a"},{"key":"harvest_source_id","value":"f0527ee7-d937-4f5a-97f2-4687fd2c7d1a"},{"key":"harvest_source_organization","value":"{\"id\": \"c1eca542-1caf-4604-a2d5-708682e08793\", \"name\": \"cioos-atlantic\", \"title\": \"SIOOC-Atlantique\", \"type\": \"organization\", \"description\": \"\", \"image_url\": \"\", \"created\": \"2026-07-31T15:58:20.870737\", \"is_organization\": true, \"approval_status\": \"approved\", \"state\": \"active\", \"description_translated\": {\"fr\": \"CIOOS-Atlantic est un consortium d\\u2019institutions partenaires engag\\u00e9es dans le d\\u00e9veloppement de la gestion et la diffusion des donn\\u00e9es oc\\u00e9anographiques de la c\\u00f4te Atlantique, du Labrador \\u00e0 la fronti\\u00e8re entre le Maine et le Nouveau-Brunswick.\\r\\n\\r\\nLa collaboration continue avec un large \\u00e9ventail de parties prenantes fait partie int\\u00e9grante de CIOOS-Atlantique, et nous travaillerons pour r\\u00e9pondre aux besoins de la communaut\\u00e9 oc\\u00e9anographique et veiller \\u00e0 ce que les int\\u00e9r\\u00eats r\\u00e9gionaux soient repr\\u00e9sent\\u00e9s au niveau national. 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Convection also transfers atmospheric gases from the surface to intermediate depths, reducing the rate of increase of carbon dioxide in the atmosphere but increasing the acidity of the ocean.\\\", \\\"edition\\\": \\\"\\\", \\\"edition-date\\\": \\\"\\\", \\\"publisher\\\": \\\"\\\", \\\"title\\\": \\\"Maritimes Region Atlantic Zone Off-Shelf Monitoring Program (AZOMP) Moored Time Series Data\\\", \\\"language\\\": \\\"en\\\", \\\"URL\\\": \\\"https://catalogue.cioosatlantic.ca/dataset/ca-cioos_348ca0d9-6de9-4bd8-9dbd-ccf89f981049?local=en\\\"}]","fr":"[{\\\"type\\\": \\\"dataset\\\", \\\"id\\\": \\\"ca.cioos_348ca0d9-6de9-4bd8-9dbd-ccf89f981049\\\", \\\"author\\\": [{\\\"given\\\": \\\"Marine\\\", \\\"family\\\": \\\"Environmental Data Section (MEDS)\\\"}], \\\"issued\\\": [{\\\"date-parts\\\": [\\\"2023\\\", \\\"08\\\", \\\"01\\\"]}], \\\"abstract\\\": \\\"Le Programme de surveillance hors plateau de la zone Atlantique (AZOMP) recueille et analyse les observations oc\\u00e9anographiques physiques, chimiques et biologiques du talus continental et des bassins profonds de l'Atlantique Nord-Ouest, dans le but global de surveiller la variabilit\\u00e9 du climat oc\\u00e9anique et du plancton affectant les \\u00e9cosyst\\u00e8mes au large du Canada atlantique et les syst\\u00e8mes climatiques \\u00e0 l'\\u00e9chelle r\\u00e9gionale et mondiale. \\n\\nLes mesures annuelles dans la mer du Labrador ont d\\u00e9but\\u00e9 en 1990 dans le cadre de l'exp\\u00e9rience mondiale sur la circulation oc\\u00e9anique (WOCE) et ont \\u00e9volu\\u00e9 pour devenir un effort de surveillance r\\u00e9gional multidisciplinaire int\\u00e9gr\\u00e9 au Programme mondial d'enqu\\u00eates hydrographiques \\u00e0 base de navires oc\\u00e9aniques (GO-SHIP).\\n\\nLe programme d'\\u00e9chantillonnage d'AZOMP au large du Canada atlantique et de la mer du Labrador comprend l'\\u00e9chantillonnage annuel de la ligne Atlantic Repeat 7-West (AR7W), une ligne de 880 km traversant la mer du Labrador depuis la c\\u00f4te du Labrador jusqu'\\u00e0 la c\\u00f4te groenlandaise et une extension de la ligne Halifax, ainsi que des stations en eau profonde au-dessus du Scotian Slope and Rise situ\\u00e9es \\u00e0 l'extr\\u00e9mit\\u00e9 de la ligne Halifax de l'AZMP. L'\\u00e9chantillonnage opportuniste peut \\u00e9galement avoir lieu \\u00e0 des stations situ\\u00e9es dans le d\\u00e9troit de Belle Ilse, \\u00e0 la station 27, sur le plateau du Labrador et sur la ligne ouest de l'OSNAP \\u00e0 l'appui de programmes et d'initiatives de recherche auxiliaires. En outre, les flotteurs XBT et Argo sont couramment d\\u00e9ploy\\u00e9s et l'ADCP mont\\u00e9 sur les navires est utilis\\u00e9 pour d\\u00e9terminer les structures des masses d'eau \\u00e0 plus petite \\u00e9chelle. Des amarres oc\\u00e9anographiques en eau profonde sont \\u00e9galement d\\u00e9ploy\\u00e9es dans la mer du Labrador, principalement dans la r\\u00e9gion de Hamilton Bank, sur la ligne ouest de l'OSNAP et sur le versant n\\u00e9o-\\u00e9cossais. Les donn\\u00e9es de s\\u00e9ries chronologiques sont utilis\\u00e9es \\u00e0 des fins de comparaison avec les estimations du transport par mod\\u00e8le num\\u00e9rique de la Nouvelle-\\u00c9cosse et du courant du Labrador. \\n\\nLes donn\\u00e9es recueillies sont synth\\u00e9tis\\u00e9es dans des rapports annuels sur les changements physiques, chimiques et biologiques dans les eaux canadiennes de l'Atlantique et de la mer du Labrador. L'un des principaux objectifs est l'\\u00e9volution de l'intensit\\u00e9 du renversement hivernal des eaux de surface et de profondeur interm\\u00e9diaire, qui entra\\u00eene la formation de masses d'eau profondes et fait partie de la circulation thermohaline qui influe sur le climat mondial. 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Labrador to the Maine / New Brunswick border.\r\n\r\nMeaningful engagement and ongoing communication with a broad variety of stakeholders is an integral component of CIOOS-Atlantic, and we will work to meet the needs of the local oceanographic community and ensure regional interests are represented at the national level. Emphasis is placed on the creation of a system which promotes easy data access and supports the work of partners, researchers, industry, and more.","fr":"CIOOS-Atlantic est un consortium d’institutions partenaires engagées dans le développement de la gestion et la diffusion des données océanographiques de la côte Atlantique, du Labrador à la frontière entre le Maine et le Nouveau-Brunswick.\r\n\r\nLa collaboration continue avec un large éventail de parties prenantes fait partie intégrante de CIOOS-Atlantique, et nous travaillerons pour répondre aux besoins de la communauté océanographique et veiller à ce que les intérêts régionaux soient représentés au niveau national. L'accent est mis sur la création d'un système qui facilite l'accès aux données afin de soutenir le travail des partenaires, chercheurs, industries, etc."}},"license_title":"government-open-license-canada","num_resources":3,"resource-type":"dataset","bbox-east-long":"-48.1","bbox-north-lat":"60.6","bbox-south-lat":"37.7","bbox-west-long":"-63.7","creator_user_id":"fe6035ee-ed91-4ead-b5b2-4048232a22bb","temporal-extent":[{"begin":"1998-01-01"}],"vertical-extent":[{"max":"5500.0","min":"1.0"}],"maintainer_email":null,"maintenance-note":"Generated from https://cioos-siooc.github.io/metadata-entry-form","metadata_created":"2026-09-04T17:28:27.606187","notes_translated":{"en":"The Atlantic Zone Off-Shelf Monitoring Program (AZOMP) collects and analyzes physical, chemical, and biological oceanographic observations from the continental slope and deep basins of the Northwest Atlantic, with the overarching goal of monitoring variability in ocean climate and plankton affecting ecosystems off Atlantic Canada and climate systems at both regional and global scales. \n\nAnnual measurements in the Labrador Sea began in 1990 as a contribution to the World Ocean Circulation Experiment (WOCE) and have evolved into a multidisciplinary regional monitoring effort and part of the Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP).\n\nAZOMP's sampling scheme off Atlantic Canada and the Labrador Sea involves annual sampling of both the Atlantic Repeat 7-West (AR7W) line, a 880 km-line running across the Labrador Sea from Labrador to Greenland coast and extended Halifax Line, deep-water stations over the Scotian Slope and Rise located at the end of AZMP’s Halifax Line. Opportunistic sampling also may occur at stations in the Strait of Belle Ilse, station 27, Labrador Shelf, and OSNAP West line in support of ancillary research programs and initiatives. In addition XBTs and Argo floats are commonly deployed and vessel-mounted ADCP is used to determine water masses structures at a smaller scale. Deep-water oceanographic moorings are also deployed in the Labrador Sea, mostly in the Hamilton Bank region and OSNAP West Line and on the Scotian Slope.   Time series data is used for comparison with the numerical model transport estimates of the Nova Scotia and the Labrador Current.  \n\nThe data collected are synthesized into annual reports on the physical, chemical and biological changes in Atlantic Canadian waters and the Labrador Sea. One primary focus is on changes in the intensity of winter overturning of surface and intermediate-depth waters resulting in deep water mass formation and is part of the thermohaline circulation that affects the global climate. Convection also transfers atmospheric gases from the surface to intermediate depths, reducing the rate of increase of carbon dioxide in the atmosphere but increasing the acidity of the ocean.","fr":"Le Programme de surveillance hors plateau de la zone Atlantique (AZOMP) recueille et analyse les observations océanographiques physiques, chimiques et biologiques du talus continental et des bassins profonds de l'Atlantique Nord-Ouest, dans le but global de surveiller la variabilité du climat océanique et du plancton affectant les écosystèmes au large du Canada atlantique et les systèmes climatiques à l'échelle régionale et mondiale. \n\nLes mesures annuelles dans la mer du Labrador ont débuté en 1990 dans le cadre de l'expérience mondiale sur la circulation océanique (WOCE) et ont évolué pour devenir un effort de surveillance régional multidisciplinaire intégré au Programme mondial d'enquêtes hydrographiques à base de navires océaniques (GO-SHIP).\n\nLe programme d'échantillonnage d'AZOMP au large du Canada atlantique et de la mer du Labrador comprend l'échantillonnage annuel de la ligne Atlantic Repeat 7-West (AR7W), une ligne de 880 km traversant la mer du Labrador depuis la côte du Labrador jusqu'à la côte groenlandaise et une extension de la ligne Halifax, ainsi que des stations en eau profonde au-dessus du Scotian Slope and Rise situées à l'extrémité de la ligne Halifax de l'AZMP. L'échantillonnage opportuniste peut également avoir lieu à des stations situées dans le détroit de Belle Ilse, à la station 27, sur le plateau du Labrador et sur la ligne ouest de l'OSNAP à l'appui de programmes et d'initiatives de recherche auxiliaires. En outre, les flotteurs XBT et Argo sont couramment déployés et l'ADCP monté sur les navires est utilisé pour déterminer les structures des masses d'eau à plus petite échelle. Des amarres océanographiques en eau profonde sont également déployées dans la mer du Labrador, principalement dans la région de Hamilton Bank, sur la ligne ouest de l'OSNAP et sur le versant néo-écossais. Les données de séries chronologiques sont utilisées à des fins de comparaison avec les estimations du transport par modèle numérique de la Nouvelle-Écosse et du courant du Labrador. \n\nLes données recueillies sont synthétisées dans des rapports annuels sur les changements physiques, chimiques et biologiques dans les eaux canadiennes de l'Atlantique et de la mer du Labrador. L'un des principaux objectifs est l'évolution de l'intensité du renversement hivernal des eaux de surface et de profondeur intermédiaire, qui entraîne la formation de masses d'eau profondes et fait partie de la circulation thermohaline qui influe sur le climat mondial. La convection transfère également les gaz atmosphériques de la surface vers des profondeurs intermédiaires, ce qui réduit le taux d'augmentation du dioxyde de carbone dans l'atmosphère mais augmente l'acidité de l'océan."},"title_translated":{"en":"Maritimes Region Atlantic Zone Off-Shelf Monitoring Program (AZOMP) Moored Time Series Data","fr":"Données chronologiques amarrées du Programme de surveillance hors plateau de la zone Atlantique (AZOMP) de la région des Maritimes"},"xml_location_url":"https://cioosatlantic.ca/metadata/dfo/bio/moored/maritimes_region_atlantic_zone_348ca.xml","metadata-language":"en","metadata_modified":"2026-09-04T17:28:27.606191","frequency-of-update":"asNeeded","dataset-reference-date":[{"type":"creation","value":"1998-01-01"}],"cited-responsible-party":[{"role":"owner","individual-name":"Environmental Data Section (MEDS), Marine","organisation-name":"Fisheries and Oceans 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Marine</gco:CharacterString>\n                      </cit:name>\n                      <cit:contactInfo>\n                        <cit:CI_Contact></cit:CI_Contact>\n                      </cit:contactInfo>\n                      <cit:positionName>\n                        <gco:CharacterString></gco:CharacterString>\n                      </cit:positionName>\n                    </cit:CI_Individual>\n                  </cit:individual>\n                </cit:CI_Organisation>\n              </cit:party>\n            </cit:CI_Responsibility>\n          </cit:citedResponsibleParty>\n        </cit:CI_Citation>\n      </mri:citation>\n      <mri:abstract xsi:type=\"lan:PT_FreeText_PropertyType\">\n        <gco:CharacterString>The Atlantic Zone Off-Shelf Monitoring Program (AZOMP) collects and analyzes physical, chemical, and biological oceanographic observations from the continental slope and deep basins of the Northwest Atlantic, with the overarching goal of monitoring variability in ocean climate and plankton affecting ecosystems off Atlantic Canada and climate systems at both regional and global scales. \n\nAnnual measurements in the Labrador Sea began in 1990 as a contribution to the World Ocean Circulation Experiment (WOCE) and have evolved into a multidisciplinary regional monitoring effort and part of the Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP).\n\nAZOMP&#39;s sampling scheme off Atlantic Canada and the Labrador Sea involves annual sampling of both the Atlantic Repeat 7-West (AR7W) line, a 880 km-line running across the Labrador Sea from Labrador to Greenland coast and extended Halifax Line, deep-water stations over the Scotian Slope and Rise located at the end of AZMP’s Halifax Line. Opportunistic sampling also may occur at stations in the Strait of Belle Ilse, station 27, Labrador Shelf, and OSNAP West line in support of ancillary research programs and initiatives. In addition XBTs and Argo floats are commonly deployed and vessel-mounted ADCP is used to determine water masses structures at a smaller scale. Deep-water oceanographic moorings are also deployed in the Labrador Sea, mostly in the Hamilton Bank region and OSNAP West Line and on the Scotian Slope.   Time series data is used for comparison with the numerical model transport estimates of the Nova Scotia and the Labrador Current.  \n\nThe data collected are synthesized into annual reports on the physical, chemical and biological changes in Atlantic Canadian waters and the Labrador Sea. One primary focus is on changes in the intensity of winter overturning of surface and intermediate-depth waters resulting in deep water mass formation and is part of the thermohaline circulation that affects the global climate. 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L&#39;échantillonnage opportuniste peut également avoir lieu à des stations situées dans le détroit de Belle Ilse, à la station 27, sur le plateau du Labrador et sur la ligne ouest de l&#39;OSNAP à l&#39;appui de programmes et d&#39;initiatives de recherche auxiliaires. En outre, les flotteurs XBT et Argo sont couramment déployés et l&#39;ADCP monté sur les navires est utilisé pour déterminer les structures des masses d&#39;eau à plus petite échelle. Des amarres océanographiques en eau profonde sont également déployées dans la mer du Labrador, principalement dans la région de Hamilton Bank, sur la ligne ouest de l&#39;OSNAP et sur le versant néo-écossais. Les données de séries chronologiques sont utilisées à des fins de comparaison avec les estimations du transport par modèle numérique de la Nouvelle-Écosse et du courant du Labrador. \n\nLes données recueillies sont synthétisées dans des rapports annuels sur les changements physiques, chimiques et biologiques dans les eaux canadiennes de l&#39;Atlantique et de la mer du Labrador. L&#39;un des principaux objectifs est l&#39;évolution de l&#39;intensité du renversement hivernal des eaux de surface et de profondeur intermédiaire, qui entraîne la formation de masses d&#39;eau profondes et fait partie de la circulation thermohaline qui influe sur le climat mondial. 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