{"help":"https://catalogue.cioos.ca/api/3/action/help_show?name=package_show","success":true,"result":{"id":"5f0ed6d7-1bf7-41ce-962a-2896e0aaa3e2","ecv":["sea_ice"],"eov":["seaIce","dissolvedOrganicCarbon"],"url":null,"name":"ca-cioos_ccin-13249","tags":[],"type":"dataset","notes":"Les concentrations dissoutes de ces gaz ont été mesurées à l'aide d'un équilibreur à serpentin à flux segmenté (SFCE) couplé à un spectromètre de masse à réaction par transfert de protons (PTR-MS). Pour plus d'informations, veuillez consulter Wohl, C., Capelle, D., Jones, A., Sturges, W.T., Nightingale, P.D., Else, B.G.T. et Yang, M. : Equilibrateur à serpentin segmenté couplé à un spectromètre de masse à réaction de transfert de protons pour les mesures d'une large gamme de composés organiques volatils dans l'eau de mer, Ocean Sci., 15, 925—940, https://doi.org/10.5194/os-15-925-2019, 2019.\n\nUne description détaillée de l'installation à bord et de l'analyse des données spécifiques à ce déploiement se trouvent dans la citation des données.\n\nEn bref, le SFCE-PTR-MS a été installé dans l'un des laboratoires situés à l'avant du navire et utilisé pour prélever des échantillons discrets à partir de profils de profondeur ou de l'eau de mer en cours d'eau provenant de l'entrée d'eau de mer principale du navire.\n\nLe navire de recherche est parti d'Iqaluit vers le nord en passant par le détroit de Davis et la baie de Baffin pour atteindre Smith Sound. 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For more information, please refer to Wohl, C., Capelle, D., Jones, A., Sturges, W. T., Nightingale, P. D., Else, B. G. T., and Yang, M.: Segmented flow coil equilibrator coupled to a proton-transfer-reaction mass spectrometer for measurements of a broad range of volatile organic compounds in seawater, Ocean Sci., 15, 925\\u2013940, https://doi.org/10.5194/os-15-925-2019, 2019.\\n\\nDetailed description of the installation on board and the data analysis specific to this deployment can be found in the data citation.\\n\\nBriefly, the SFCE-PTR-MS was set up in one of the labs near the front of the ship and used to sample either discrete samples from depth profiles or underway seawater from the main seawater inlet of the ship.\\n\\nThe research vessel travelled from Iqaluit northwards through Davis Strait and Baffin Bay to reach Smith Sound. In this area, more intense depth profile sampling was carried out. The vessel then travelled to Pond Inlet and Resolute. Sampling ended south of Resolute in Peel Sound.\\n\\nDepth profiles of dissolved gas concentrations were measured from the Rosette-mounted Niskin bottles as discrete samples from the near surface (about 2 m) to 60 m depth at a total of 21 stations as per availability. The exact sampling depth as determined by the CTD crew is listed in the \\\\\"CTD concentrations\\\\\" data file.\\n\\nWhen logistically feasible at station, a handheld vertical 5 dm^(3) Niskin bottle was deployed off the front starboard side of the ship to sample approximately the top 30 cm from the ocean surface. This was done by bringing the Niskin bottle up from approximately 3 m and firing it just before it reached the surface using rope marks as depth indicators, similar to described in Ahmed et al. (2020). Samples collected with this method are marked as sampled from 0.3 m in the \\\\\"CTD concentrations\\\\\" data file. The AMSR2 passive microwave sea ice concentration (SIC) satellite product (daily, 3.125 km x 3,125 km resolution) (Spreen et al., 2008) was used to create a time series of sea ice concentration along the cruise track.\\\", \\\"edition-date\\\": \\\"\\\", \\\"publisher\\\": \\\"\\\", \\\"title\\\": \\\"Shipborne Dissolved Organic Gas Measurements in Depth Profiles and Underway Seawater (Methanol, Acetone, Acetaldehyde, DMS, Isoprene) Amundsen 2017\\\", \\\"version\\\": \\\"1.0\\\", \\\"DOI\\\": \\\"10.21963/13249\\\", \\\"language\\\": \\\"en\\\", \\\"URL\\\": \\\"https://catalogue.cioos.ca/dataset/ca-cioos_ccin-13249?local=en\\\"}]","fr":"[{\\\"type\\\": \\\"dataset\\\", \\\"id\\\": \\\"ca.cioos_ccin-13249\\\", \\\"author\\\": [{\\\"given\\\": \\\"Yang\\\", \\\"family\\\": \\\"Mingxi\\\"}, {\\\"given\\\": \\\"Charel\\\", \\\"family\\\": \\\"Wohl\\\"}, {\\\"given\\\": \\\"Brian\\\", \\\"family\\\": \\\"Butterworth\\\"}, {\\\"given\\\": \\\"Brent\\\", \\\"family\\\": \\\"Else\\\"}, {\\\"given\\\": \\\"Anna\\\", \\\"family\\\": \\\"Jones\\\"}, {\\\"given\\\": \\\"Philip\\\", \\\"family\\\": \\\"Nightingale\\\"}, {\\\"given\\\": \\\"William\\\", \\\"family\\\": \\\"Sturges\\\"}], \\\"issued\\\": [{\\\"date-parts\\\": [\\\"2024\\\", \\\"07\\\", \\\"18\\\"]}], \\\"abstract\\\": \\\"Les concentrations dissoutes de ces gaz ont \\u00e9t\\u00e9 mesur\\u00e9es \\u00e0 l'aide d'un \\u00e9quilibreur \\u00e0 serpentin \\u00e0 flux segment\\u00e9 (SFCE) coupl\\u00e9 \\u00e0 un spectrom\\u00e8tre de masse \\u00e0 r\\u00e9action par transfert de protons (PTR-MS). Pour plus d'informations, veuillez consulter Wohl, C., Capelle, D., Jones, A., Sturges, W.T., Nightingale, P.D., Else, B.G.T. et Yang, M.\\u00a0: Equilibrateur \\u00e0 serpentin segment\\u00e9 coupl\\u00e9 \\u00e0 un spectrom\\u00e8tre de masse \\u00e0 r\\u00e9action de transfert de protons pour les mesures d'une large gamme de compos\\u00e9s organiques volatils dans l'eau de mer, Ocean Sci., 15, 925\\u2014940, https://doi.org/10.5194/os-15-925-2019, 2019.\\n\\nUne description d\\u00e9taill\\u00e9e de l'installation \\u00e0 bord et de l'analyse des donn\\u00e9es sp\\u00e9cifiques \\u00e0 ce d\\u00e9ploiement se trouvent dans la citation des donn\\u00e9es.\\n\\nEn bref, le SFCE-PTR-MS a \\u00e9t\\u00e9 install\\u00e9 dans l'un des laboratoires situ\\u00e9s \\u00e0 l'avant du navire et utilis\\u00e9 pour pr\\u00e9lever des \\u00e9chantillons discrets \\u00e0 partir de profils de profondeur ou de l'eau de mer en cours d'eau provenant de l'entr\\u00e9e d'eau de mer principale du navire.\\n\\nLe navire de recherche est parti d'Iqaluit vers le nord en passant par le d\\u00e9troit de Davis et la baie de Baffin pour atteindre Smith Sound. Dans cette zone, un \\u00e9chantillonnage plus intense du profil de profondeur a \\u00e9t\\u00e9 effectu\\u00e9. Le navire s'est ensuite rendu \\u00e0 Pond Inlet et \\u00e0 Resolute. L'\\u00e9chantillonnage s'est termin\\u00e9 au sud de Resolute, dans le d\\u00e9troit de Peel.\\n\\nLes profils de profondeur des concentrations de gaz dissous ont \\u00e9t\\u00e9 mesur\\u00e9s \\u00e0 partir des bouteilles Niskin mont\\u00e9es sur Rosette sous forme d'\\u00e9chantillons discrets pr\\u00e9lev\\u00e9s pr\\u00e8s de la surface (environ 2 m) \\u00e0 60 m de profondeur dans un total de 21 stations selon la disponibilit\\u00e9. La profondeur d'\\u00e9chantillonnage exacte d\\u00e9termin\\u00e9e par l'\\u00e9quipe du CTD est r\\u00e9pertori\\u00e9e dans le fichier de donn\\u00e9es \\u00ab\\u00a0Concentrations de CTD\\u00a0\\u00bb.\\n\\nLorsque la logistique le permettait \\u00e0 la station, une bouteille Niskin verticale portative de 5 dm^ (3) a \\u00e9t\\u00e9 d\\u00e9ploy\\u00e9e sur le c\\u00f4t\\u00e9 avant tribord du navire pour pr\\u00e9lever des \\u00e9chantillons \\u00e0 environ 30 cm de la surface de l'oc\\u00e9an. Cela a \\u00e9t\\u00e9 fait en soulevant la bouteille Niskin d'environ 3 m et en la tirant juste avant qu'elle n'atteigne la surface en utilisant des marques de corde comme indicateurs de profondeur, comme d\\u00e9crit dans Ahmed et al. (2020). Les \\u00e9chantillons pr\\u00e9lev\\u00e9s selon cette m\\u00e9thode sont marqu\\u00e9s comme \\u00e9tant \\u00e9chantillonn\\u00e9s \\u00e0 0,3 m dans le fichier de donn\\u00e9es \\u00ab\\u00a0Concentrations de CTD\\u00a0\\u00bb. Le produit satellite passif \\u00e0 micro-ondes sur la concentration de glace de mer (SIC) AMSR2 (r\\u00e9solution quotidienne de 3,125 km x 3 125 km) (Spreen et al., 2008) a \\u00e9t\\u00e9 utilis\\u00e9 pour cr\\u00e9er une s\\u00e9rie chronologique de la concentration de glace de mer le long de la trajectoire de croisi\\u00e8re.\\\", \\\"edition-date\\\": \\\"\\\", \\\"publisher\\\": \\\"\\\", \\\"title\\\": \\\"Mesures des gaz organiques dissous \\u00e0 bord des navires dans les profils de profondeur et dans l'eau de mer en cours d'eau (m\\u00e9thanol, ac\\u00e9tone, ac\\u00e9tald\\u00e9hyde, DMS, isopr\\u00e8ne) Amundsen 2017\\\", \\\"version\\\": \\\"1.0\\\", \\\"DOI\\\": \\\"10.21963/13249\\\", \\\"language\\\": \\\"fr\\\", \\\"URL\\\": \\\"https://catalogue.cioos.ca/dataset/ca-cioos_ccin-13249?local=fr\\\"}]"},"keywords":{"en":["oceans","davis-strait---oaeek","dimethylsulfide-dms","air-gas-exchange","smith-sound---oapgf","baffin-bay---oabmi","biogeochemistry","sea-ice","organic-carbon","amundsen-science-amundsen-science","seaice","dissolvedorganiccarbon"],"fr":["amundsen-science-amundsen-science","glace-de-mer","carbone-organique-dissous"]},"num_tags":0,"progress":"completed","projects":["Amundsen Science-Amundsen Science"],"owner_org":"ebfcf2b6-dac6-418e-9193-f995479939a1","resources":[{"id":"37abab79-8801-47cf-a000-5312fb504607","url":"https://docs.google.com/forms/d/e/1FAIpQLSdvBGLgaXHF1auiYcF2cKuoZzVTVevtkyUyL5lKSBq3DlN2Fg/viewform?usp=pp_url&entry.1112188064=https%3A%2F%2Fcatalogue.amundsenscience.com%2Fdataset%2Fca-cioos_ccin-13249&entry.1881810302=%5B%7B%22givenNames%22%3A%20%22Charel%22%2C%20%22lastName%22%3A%20%22Wohl%22%2C%20%22indEmail%22%3A%20%22charel.wohl%40gmail.com%22%2C%20%22orgName%22%3A%20%22Plymouth%20Marine%20Laboratory%20%2F%20Institud%20de%20Ciences%20del%20Mar%22%2C%20%22orgEmail%22%3A%20%22%22%7D%5D","hash":"","name":"Formulaire de demande d'accès aux données","size":null,"state":"active","format":"HTML","created":"2026-10-26T01:45:09.341416","mimetype":null,"position":0,"url_type":null,"cache_url":null,"package_id":"5f0ed6d7-1bf7-41ce-962a-2896e0aaa3e2","description":"Les données ne sont pas accessibles publiquement. 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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":"-57.8573","bbox-north-lat":"78.3282","bbox-south-lat":"62.0281","bbox-west-long":"-100.035","creator_user_id":"fe6035ee-ed91-4ead-b5b2-4048232a22bb","temporal-extent":[{"end":"2017-08-04","begin":"2017-07-15"}],"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=13249"}],"maintainer_email":null,"maintenance-note":"Generated from https://cioos-siooc.github.io/metadata-entry-form#/en/amundsen/c8GqCtwH6sZnf3HtZhCgkOsmtoh1/ccin-13249","metadata_created":"2026-10-26T01:45:09.339931","notes_translated":{"en":"Dissolved concentrations of these gases were measured using a segmented flow coil equilibrator (SFCE) coupled to a Proton Transfer Reaction Mass Spectrometer (PTR-MS). For more information, please refer to Wohl, C., Capelle, D., Jones, A., Sturges, W. T., Nightingale, P. D., Else, B. G. T., and Yang, M.: Segmented flow coil equilibrator coupled to a proton-transfer-reaction mass spectrometer for measurements of a broad range of volatile organic compounds in seawater, Ocean Sci., 15, 925–940, https://doi.org/10.5194/os-15-925-2019, 2019.\n\nDetailed description of the installation on board and the data analysis specific to this deployment can be found in the data citation.\n\nBriefly, the SFCE-PTR-MS was set up in one of the labs near the front of the ship and used to sample either discrete samples from depth profiles or underway seawater from the main seawater inlet of the ship.\n\nThe research vessel travelled from Iqaluit northwards through Davis Strait and Baffin Bay to reach Smith Sound. In this area, more intense depth profile sampling was carried out. The vessel then travelled to Pond Inlet and Resolute. Sampling ended south of Resolute in Peel Sound.\n\nDepth profiles of dissolved gas concentrations were measured from the Rosette-mounted Niskin bottles as discrete samples from the near surface (about 2 m) to 60 m depth at a total of 21 stations as per availability. The exact sampling depth as determined by the CTD crew is listed in the \"CTD concentrations\" data file.\n\nWhen logistically feasible at station, a handheld vertical 5 dm^(3) Niskin bottle was deployed off the front starboard side of the ship to sample approximately the top 30 cm from the ocean surface. This was done by bringing the Niskin bottle up from approximately 3 m and firing it just before it reached the surface using rope marks as depth indicators, similar to described in Ahmed et al. (2020). Samples collected with this method are marked as sampled from 0.3 m in the \"CTD concentrations\" data file. The AMSR2 passive microwave sea ice concentration (SIC) satellite product (daily, 3.125 km x 3,125 km resolution) (Spreen et al., 2008) was used to create a time series of sea ice concentration along the cruise track.","fr":"Les concentrations dissoutes de ces gaz ont été mesurées à l'aide d'un équilibreur à serpentin à flux segmenté (SFCE) couplé à un spectromètre de masse à réaction par transfert de protons (PTR-MS). Pour plus d'informations, veuillez consulter Wohl, C., Capelle, D., Jones, A., Sturges, W.T., Nightingale, P.D., Else, B.G.T. et Yang, M. : Equilibrateur à serpentin segmenté couplé à un spectromètre de masse à réaction de transfert de protons pour les mesures d'une large gamme de composés organiques volatils dans l'eau de mer, Ocean Sci., 15, 925—940, https://doi.org/10.5194/os-15-925-2019, 2019.\n\nUne description détaillée de l'installation à bord et de l'analyse des données spécifiques à ce déploiement se trouvent dans la citation des données.\n\nEn bref, le SFCE-PTR-MS a été installé dans l'un des laboratoires situés à l'avant du navire et utilisé pour prélever des échantillons discrets à partir de profils de profondeur ou de l'eau de mer en cours d'eau provenant de l'entrée d'eau de mer principale du navire.\n\nLe navire de recherche est parti d'Iqaluit vers le nord en passant par le détroit de Davis et la baie de Baffin pour atteindre Smith Sound. Dans cette zone, un échantillonnage plus intense du profil de profondeur a été effectué. Le navire s'est ensuite rendu à Pond Inlet et à Resolute. L'échantillonnage s'est terminé au sud de Resolute, dans le détroit de Peel.\n\nLes profils de profondeur des concentrations de gaz dissous ont été mesurés à partir des bouteilles Niskin montées sur Rosette sous forme d'échantillons discrets prélevés près de la surface (environ 2 m) à 60 m de profondeur dans un total de 21 stations selon la disponibilité. La profondeur d'échantillonnage exacte déterminée par l'équipe du CTD est répertoriée dans le fichier de données « Concentrations de CTD ».\n\nLorsque la logistique le permettait à la station, une bouteille Niskin verticale portative de 5 dm^ (3) a été déployée sur le côté avant tribord du navire pour prélever des échantillons à environ 30 cm de la surface de l'océan. Cela a été fait en soulevant la bouteille Niskin d'environ 3 m et en la tirant juste avant qu'elle n'atteigne la surface en utilisant des marques de corde comme indicateurs de profondeur, comme décrit dans Ahmed et al. (2020). Les échantillons prélevés selon cette méthode sont marqués comme étant échantillonnés à 0,3 m dans le fichier de données « Concentrations de CTD ». Le produit satellite passif à micro-ondes sur la concentration de glace de mer (SIC) AMSR2 (résolution quotidienne de 3,125 km x 3 125 km) (Spreen et al., 2008) a été utilisé pour créer une série chronologique de la concentration de glace de mer le long de la trajectoire de croisière."},"title_translated":{"en":"Shipborne Dissolved Organic Gas Measurements in Depth Profiles and Underway Seawater (Methanol, Acetone, Acetaldehyde, DMS, Isoprene) Amundsen 2017","fr":"Mesures des gaz organiques dissous à bord des navires dans les profils de profondeur et dans l'eau de mer en cours d'eau (méthanol, acétone, acétaldéhyde, DMS, isoprène) Amundsen 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flow coil equilibrator (SFCE) coupled to a Proton Transfer Reaction Mass Spectrometer (PTR-MS). For more information, please refer to Wohl, C., Capelle, D., Jones, A., Sturges, W. T., Nightingale, P. D., Else, B. G. T., and Yang, M.: Segmented flow coil equilibrator coupled to a proton-transfer-reaction mass spectrometer for measurements of a broad range of volatile organic compounds in seawater, Ocean Sci., 15, 925–940, https://doi.org/10.5194/os-15-925-2019, 2019.\n\nDetailed description of the installation on board and the data analysis specific to this deployment can be found in the data citation.\n\nBriefly, the SFCE-PTR-MS was set up in one of the labs near the front of the ship and used to sample either discrete samples from depth profiles or underway seawater from the main seawater inlet of the ship.\n\nThe research vessel travelled from Iqaluit northwards through Davis Strait and Baffin Bay to reach Smith Sound. In this area, more intense depth profile sampling was carried out. The vessel then travelled to Pond Inlet and Resolute. Sampling ended south of Resolute in Peel Sound.\n\nDepth profiles of dissolved gas concentrations were measured from the Rosette-mounted Niskin bottles as discrete samples from the near surface (about 2 m) to 60 m depth at a total of 21 stations as per availability. The exact sampling depth as determined by the CTD crew is listed in the &#34;CTD concentrations&#34; data file.\n\nWhen logistically feasible at station, a handheld vertical 5 dm^(3) Niskin bottle was deployed off the front starboard side of the ship to sample approximately the top 30 cm from the ocean surface. This was done by bringing the Niskin bottle up from approximately 3 m and firing it just before it reached the surface using rope marks as depth indicators, similar to described in Ahmed et al. (2020). Samples collected with this method are marked as sampled from 0.3 m in the &#34;CTD concentrations&#34; data file. The AMSR2 passive microwave sea ice concentration (SIC) satellite product (daily, 3.125 km x 3,125 km resolution) (Spreen et al., 2008) was used to create a time series of sea ice concentration along the cruise track.</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 concentrations dissoutes de ces gaz ont été mesurées à l&#39;aide d&#39;un équilibreur à serpentin à flux segmenté (SFCE) couplé à un spectromètre de masse à réaction par transfert de protons (PTR-MS). Pour plus d&#39;informations, veuillez consulter Wohl, C., Capelle, D., Jones, A., Sturges, W.T., Nightingale, P.D., Else, B.G.T. et Yang, M. : Equilibrateur à serpentin segmenté couplé à un spectromètre de masse à réaction de transfert de protons pour les mesures d&#39;une large gamme de composés organiques volatils dans l&#39;eau de mer, Ocean Sci., 15, 925—940, https://doi.org/10.5194/os-15-925-2019, 2019.\n\nUne description détaillée de l&#39;installation à bord et de l&#39;analyse des données spécifiques à ce déploiement se trouvent dans la citation des données.\n\nEn bref, le SFCE-PTR-MS a été installé dans l&#39;un des laboratoires situés à l&#39;avant du navire et utilisé pour prélever des échantillons discrets à partir de profils de profondeur ou de l&#39;eau de mer en cours d&#39;eau provenant de l&#39;entrée d&#39;eau de mer principale du navire.\n\nLe navire de recherche est parti d&#39;Iqaluit vers le nord en passant par le détroit de Davis et la baie de Baffin pour atteindre Smith Sound. Dans cette zone, un échantillonnage plus intense du profil de profondeur a été effectué. Le navire s&#39;est ensuite rendu à Pond Inlet et à Resolute. L&#39;échantillonnage s&#39;est terminé au sud de Resolute, dans le détroit de Peel.\n\nLes profils de profondeur des concentrations de gaz dissous ont été mesurés à partir des bouteilles Niskin montées sur Rosette sous forme d&#39;échantillons discrets prélevés près de la surface (environ 2 m) à 60 m de profondeur dans un total de 21 stations selon la disponibilité. La profondeur d&#39;échantillonnage exacte déterminée par l&#39;équipe du CTD est répertoriée dans le fichier de données « Concentrations de CTD ».\n\nLorsque la logistique le permettait à la station, une bouteille Niskin verticale portative de 5 dm^ (3) a été déployée sur le côté avant tribord du navire pour prélever des échantillons à environ 30 cm de la surface de l&#39;océan. Cela a été fait en soulevant la bouteille Niskin d&#39;environ 3 m et en la tirant juste avant qu&#39;elle n&#39;atteigne la surface en utilisant des marques de corde comme indicateurs de profondeur, comme décrit dans Ahmed et al. (2020). Les échantillons prélevés selon cette méthode sont marqués comme étant échantillonnés à 0,3 m dans le fichier de données « Concentrations de CTD ». 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