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Title {'en': 'Water column CO2 system measurements collected during the 2016 National Oceanic and Atmospheric Administration West Coast Ocean Acidification survey (NOAA WCOA2016) from California to British Columbia', 'fr': "Mesures du système de CO2 de la colonne d'eau recueillies lors de l'enquête sur l'acidification des océans de la côte ouest de la National Oceanic and Atmospheric Administration (NOAA WCOA2016) de la Californie à la Colombie-Britannique"}
URL ca-cioos_17396d02-88ff-4240-837b-5d3a45e70ea0
Description {'en': 'Carbon dioxide partial pressure (pCO2) and total dissolved inorganic carbon (TCO2) measurements were made on seawater collected from 12 depths at select stations occupied during the 2016 National Oceanic and Atmospheric Administration West Coast Ocean Acidification survey (NOAA WCOA2016) from California to British Columbia. NOAA cruise data collected during this survey are available from the National Centers for Environmental Information (https://www.nodc.noaa.gov/ocads/oceans/Coastal/WCOA.html). Hakai Institute staff (Evans) collected data only during the second leg of the survey from May 24 to June 7. Information describing the cruise plan and cruise blog can be found on the NOAA Pacific Marine Environmental Laboratory (PMEL) website (https://www.pmel.noaa.gov/co2/story/2016+West+Coast+Ocean+Acidification+Cruise). Seawater sampling during this cruise was conducted using a conductivity-temperature-depth (CTD) profiler coupled with a 24-Niskin (11-L) bottle rosette. Seawater collection was concentrated in the upper 200 m at standard depths: 3 m, 10 m, 20 m, 30 m, 50 m, 80 m, 100 m, 125 m, 150 m, and 200 m. Two additional deeper depths were sampled when the water column exceeded 200 m. Additional shallow depths were sampled at the Hakai Institute’s oceanographic station QU39 (http://dx.doi.org/10.21966/1.715738). Samples were drawn from the Niskin bottles with care not to introduce bubbles into 350 mL amber glass bottles using silicone tubing, and left with 3 mL of headspace. Samples were then fixed with 200 µL of mercuric chloride and crimp-sealed with polyethylene-lined metal caps. Samples were stored in the dark and at room temperature until analysis on the Hakai Institute’s Burke-o-Lator (BoL). For detailed protocols on data processing including CO2 system determination, and quality assurance, please see Pocock et al. (2017; http://dx.doi.org/10.21966/1.521066). Final CO2 system parameters (pHT, pCO2, and aragonite saturature state) were computed using (primary) CTD temperature and salinity, and BoL determined total CO2 (TCO2) corrected using certified reference materials and alkalinity (Alk) using the carbonic acid dissociation constants of Lueker et al. (2000). Calculations were done relative to in situ pressure. Note Alk here is assumed here to consist of carbonate, bicarbonate, borate, hydroxide, and hydrogen ions; neglecting the influence of nutrients and organic acids. The effort to collect these data are part of the Hakai Institute’s directive to advance the understanding of carbon cycling in northeast Pacific coastal settings with specific emphasis on ocean acidification.', 'fr': "Des mesures de pression partielle de dioxyde de carbone (pCO2) et de carbone inorganique dissous total (TCO2) ont été effectuées sur de l'eau de mer prélevée à 12 profondeurs à des stations sélectionnées occupées pendant l'enquête sur l'acidification des océans de la côte ouest de la National Oceanic and Atmospheric Administration (NOAA WCOA2016) de la Californie à Colombie-Britannique. Les données sur les croisières de la NOAA recueillies au cours de cette enquête sont disponibles auprès des National Centers for Environmental Information (https://www.nodc.noaa.gov/ocads/oceans/Coastal/WCOA.html). Le personnel de l'Institut Hakai (Evans) n'a collecté des données que lors de la deuxième partie de l'enquête, du 24 mai au 7 juin. Les informations décrivant le plan de croisière et le blog de la croisière sont disponibles sur le site Web du Laboratoire environnemental marin du Pacifique (PMEL) de la NOAA (https://www.pmel.noaa.gov/co2/story/2016+West+Coast+Ocean+Acidification+Cruise). L'échantillonnage de l'eau de mer au cours de cette croisière a été effectué à l'aide d'un profileur de conductivité-température-profondeur (CTD) couplé à une rosette de 24 bouteilles Niskin (11 L). La collecte d'eau de mer a été concentrée dans les 200 m supérieurs à des profondeurs standard\xa0: 3 m, 10 m, 20 m, 30 m, 50 m, 80 m, 100 m, 125 m, 150 m et 200 m. Deux autres profondeurs plus profondes ont été échantillonnées lorsque la colonne d'eau dépassait 200 m. Des profondeurs peu profondes supplémentaires ont été échantillonnées à la station océanographique QU39 de l'Institut Hakai (http://dx.doi.org/10.21966/1.715738). Des échantillons ont été prélevés dans les bouteilles Niskin en prenant soin de ne pas introduire de bulles dans des bouteilles en verre ambré de 350 mL à l'aide d'un tube en silicone, et laissés avec 3 mL d'espace libre. Les échantillons ont ensuite été fixés avec 200 µL de chlorure mercurique et scellés par sertissage à l'aide de bouchons métalliques doublés de polyéthylène. Les échantillons ont été conservés dans l'obscurité et à température ambiante jusqu'à l'analyse sur le Burke-o-Lator (BoL) de l'Institut Hakai. Pour des protocoles détaillés sur le traitement des données, y compris la détermination du système CO2 et l'assurance qualité, veuillez consulter Pocock et al. (2017\xa0; http://dx.doi.org/10.21966/1.521066). Les paramètres finaux du système de CO2 (pHT, pCO2 et état de saturation de l'aragonite) ont été calculés à l'aide de la température et de la salinité CTD (primaires), et le BoL a déterminé le CO2 total (TCO2) corrigé à l'aide de matériaux de référence certifiés et l'alcalinité (Alk) en utilisant les constantes de dissociation de l'acide carbonique de Lueker et al. (2000). Les calculs ont été effectués par rapport à la pression in situ. Remarque Ici, Alk est supposé être constitué d'ions carbonate, bicarbonate, borate, hydroxyde et hydrogène, sans tenir compte de l'influence des nutriments et des acides organiques. L'effort de collecte de ces données fait partie de la directive de l'Institut Hakai visant à faire progresser la compréhension du cycle du carbone dans les zones côtières du nord-est du Pacifique, avec un accent particulier sur l'acidification des océans."}
Keywords {'en': ['oceans', 'geoscientificinformation', 'co2', 'oceans', 'water', 'west-coast', 'ocean-acidification', 'other', 'inorganiccarbon'], 'fr': ['carbone-inorganique']}
Ocean Variables
  • Inorganic Carbon
  • Other
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License CC-BY-4.0
Scope Dataset
Status On Going
Topic Category oceans
Associated Datasets
Metadata Dates
Metadata Date 1
Date
2022-01-13
Type
Revision
Metadata Date 2
Date
2022-01-24
Type
Publication
Resource Dates
Resource Date 1
Date
2018-09-09
Type
Publication
Maintenance and update frequency As Needed
Maintenance Note Generated from https://cioos-siooc.github.io/metadata-entry-form
Point of Contact
Point of Contact 1
Name
Wiley Evans
Affiliation
Hakai Institute
Email
data@hakai.org
Role
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  • Point of Contact
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Responsible Party 1
Name
Wiley Evans
Affiliation
Hakai Institute
Email
data@hakai.org
Role
Owner
Responsible Party 2
Affiliation
Hakai Institute
Email
data@hakai.org
Role
Resource Provider
Distributor
Distributor 1
Affiliation
Hakai Institute
Email
data@hakai.org
Role
Distributor
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Temporal Extent
Vertical Extent
Min
0.0
Max
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Default Locale English
Citation identifier
Code
10.21966/1.715784
XML Metadata File Location https://pac-dev1.cioos.org/dev/metadata/hakai/water_column_co2_system_measur_17396.xml
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</mri:citation> <mri:abstract xsi:type="lan:PT_FreeText_PropertyType"> <gco:CharacterString>Carbon dioxide partial pressure (pCO2) and total dissolved inorganic carbon (TCO2) measurements were made on seawater collected from 12 depths at select stations occupied during the 2016 National Oceanic and Atmospheric Administration West Coast Ocean Acidification survey (NOAA WCOA2016) from California to British Columbia. NOAA cruise data collected during this survey are available from the National Centers for Environmental Information (https://www.nodc.noaa.gov/ocads/oceans/Coastal/WCOA.html). Hakai Institute staff (Evans) collected data only during the second leg of the survey from May 24 to June 7. Information describing the cruise plan and cruise blog can be found on the NOAA Pacific Marine Environmental Laboratory (PMEL) website (https://www.pmel.noaa.gov/co2/story/2016+West+Coast+Ocean+Acidification+Cruise). Seawater sampling during this cruise was conducted using a conductivity-temperature-depth (CTD) profiler coupled with a 24-Niskin (11-L) bottle rosette. Seawater collection was concentrated in the upper 200 m at standard depths: 3 m, 10 m, 20 m, 30 m, 50 m, 80 m, 100 m, 125 m, 150 m, and 200 m. Two additional deeper depths were sampled when the water column exceeded 200 m. Additional shallow depths were sampled at the Hakai Institute’s oceanographic station QU39 (http://dx.doi.org/10.21966/1.715738). Samples were drawn from the Niskin bottles with care not to introduce bubbles into 350 mL amber glass bottles using silicone tubing, and left with 3 mL of headspace. Samples were then fixed with 200 µL of mercuric chloride and crimp-sealed with polyethylene-lined metal caps. Samples were stored in the dark and at room temperature until analysis on the Hakai Institute’s Burke-o-Lator (BoL). For detailed protocols on data processing including CO2 system determination, and quality assurance, please see Pocock et al. (2017; http://dx.doi.org/10.21966/1.521066). Final CO2 system parameters (pHT, pCO2, and aragonite saturature state) were computed using (primary) CTD temperature and salinity, and BoL determined total CO2 (TCO2) corrected using certified reference materials and alkalinity (Alk) using the carbonic acid dissociation constants of Lueker et al. (2000). Calculations were done relative to in situ pressure. Note Alk here is assumed here to consist of carbonate, bicarbonate, borate, hydroxide, and hydrogen ions; neglecting the influence of nutrients and organic acids. The effort to collect these data are part of the Hakai Institute’s directive to advance the understanding of carbon cycling in northeast Pacific coastal settings with specific emphasis on ocean acidification.</gco:CharacterString> <lan:PT_FreeText> <lan:textGroup> <lan:LocalisedCharacterString locale="#fr">Des mesures de pression partielle de dioxyde de carbone (pCO2) et de carbone inorganique dissous total (TCO2) ont été effectuées sur de l&#39;eau de mer prélevée à 12 profondeurs à des stations sélectionnées occupées pendant l&#39;enquête sur l&#39;acidification des océans de la côte ouest de la National Oceanic and Atmospheric Administration (NOAA WCOA2016) de la Californie à Colombie-Britannique. Les données sur les croisières de la NOAA recueillies au cours de cette enquête sont disponibles auprès des National Centers for Environmental Information (https://www.nodc.noaa.gov/ocads/oceans/Coastal/WCOA.html). Le personnel de l&#39;Institut Hakai (Evans) n&#39;a collecté des données que lors de la deuxième partie de l&#39;enquête, du 24 mai au 7 juin. Les informations décrivant le plan de croisière et le blog de la croisière sont disponibles sur le site Web du Laboratoire environnemental marin du Pacifique (PMEL) de la NOAA (https://www.pmel.noaa.gov/co2/story/2016+West+Coast+Ocean+Acidification+Cruise). L&#39;échantillonnage de l&#39;eau de mer au cours de cette croisière a été effectué à l&#39;aide d&#39;un profileur de conductivité-température-profondeur (CTD) couplé à une rosette de 24 bouteilles Niskin (11 L). La collecte d&#39;eau de mer a été concentrée dans les 200 m supérieurs à des profondeurs standard : 3 m, 10 m, 20 m, 30 m, 50 m, 80 m, 100 m, 125 m, 150 m et 200 m. Deux autres profondeurs plus profondes ont été échantillonnées lorsque la colonne d&#39;eau dépassait 200 m. Des profondeurs peu profondes supplémentaires ont été échantillonnées à la station océanographique QU39 de l&#39;Institut Hakai (http://dx.doi.org/10.21966/1.715738). Des échantillons ont été prélevés dans les bouteilles Niskin en prenant soin de ne pas introduire de bulles dans des bouteilles en verre ambré de 350 mL à l&#39;aide d&#39;un tube en silicone, et laissés avec 3 mL d&#39;espace libre. Les échantillons ont ensuite été fixés avec 200 µL de chlorure mercurique et scellés par sertissage à l&#39;aide de bouchons métalliques doublés de polyéthylène. Les échantillons ont été conservés dans l&#39;obscurité et à température ambiante jusqu&#39;à l&#39;analyse sur le Burke-o-Lator (BoL) de l&#39;Institut Hakai. Pour des protocoles détaillés sur le traitement des données, y compris la détermination du système CO2 et l&#39;assurance qualité, veuillez consulter Pocock et al. (2017 ; http://dx.doi.org/10.21966/1.521066). Les paramètres finaux du système de CO2 (pHT, pCO2 et état de saturation de l&#39;aragonite) ont été calculés à l&#39;aide de la température et de la salinité CTD (primaires), et le BoL a déterminé le CO2 total (TCO2) corrigé à l&#39;aide de matériaux de référence certifiés et l&#39;alcalinité (Alk) en utilisant les constantes de dissociation de l&#39;acide carbonique de Lueker et al. (2000). Les calculs ont été effectués par rapport à la pression in situ. Remarque Ici, Alk est supposé être constitué d&#39;ions carbonate, bicarbonate, borate, hydroxyde et hydrogène, sans tenir compte de l&#39;influence des nutriments et des acides organiques. 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Organization 8098fd34-269d-46b0-b2a3-5349e3f6475e
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Initial dataset map max zoom level
Projects