Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ...

Data from autonomous, drifting buoy with a floating chamber to measure air-sea CO2 fluxes and gas transfer velocities (k) with high temporal and spatial resolution. The buoy is equipped with a sensor to measure aqueous and atmospheric pCO2, and to monitor the increase or loss of CO2 inside the chamb...

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Main Authors: Banko-Kubis, Hanne, Wurl, Oliver, Ribas-Ribas, Mariana
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2019
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.900728
https://doi.pangaea.de/10.1594/PANGAEA.900728
id ftdatacite:10.1594/pangaea.900728
record_format openpolar
spelling ftdatacite:10.1594/pangaea.900728 2024-09-15T18:23:31+00:00 Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ... Banko-Kubis, Hanne Wurl, Oliver Ribas-Ribas, Mariana 2019 application/zip https://dx.doi.org/10.1594/pangaea.900728 https://doi.pangaea.de/10.1594/PANGAEA.900728 en eng PANGAEA https://dx.doi.org/10.1038/s41598-019-42911-6 https://dx.doi.org/10.1016/j.oceano.2019.04.002 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Air-sea CO2 flux Fjord gas exchange gas transfer velocity marine carbon cycle ocean technology partial pressure of carbon dioxide article Collection Publication Series of Datasets 2019 ftdatacite https://doi.org/10.1594/pangaea.90072810.1038/s41598-019-42911-610.1016/j.oceano.2019.04.002 2024-07-03T13:11:36Z Data from autonomous, drifting buoy with a floating chamber to measure air-sea CO2 fluxes and gas transfer velocities (k) with high temporal and spatial resolution. The buoy is equipped with a sensor to measure aqueous and atmospheric pCO2, and to monitor the increase or loss of CO2 inside the chamber. One complete cycle including two chamber measurements last 70 minutes. The buoy can be deployed for more than 15 hours, and at wind speeds of up to 10 m/s. Floating chambers are known to overestimate fluxes due to the creation of additional turbulence at the water surface. We check that by measuring turbulence with two Acoustic Doppler Velocimeter, one directly underneath the center of the floating chamber (equipped with an inertial motion unit) and the other one positioned sideways to measure turbulence outside the perimeter of the buoy. To control the conditions below the floating chamber, a sensor which measures temperature, pressure and humidity was installed inside the chamber. ... Article in Journal/Newspaper North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Air-sea CO2 flux
Fjord
gas exchange
gas transfer velocity
marine carbon cycle
ocean technology
partial pressure of carbon dioxide
spellingShingle Air-sea CO2 flux
Fjord
gas exchange
gas transfer velocity
marine carbon cycle
ocean technology
partial pressure of carbon dioxide
Banko-Kubis, Hanne
Wurl, Oliver
Ribas-Ribas, Mariana
Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ...
topic_facet Air-sea CO2 flux
Fjord
gas exchange
gas transfer velocity
marine carbon cycle
ocean technology
partial pressure of carbon dioxide
description Data from autonomous, drifting buoy with a floating chamber to measure air-sea CO2 fluxes and gas transfer velocities (k) with high temporal and spatial resolution. The buoy is equipped with a sensor to measure aqueous and atmospheric pCO2, and to monitor the increase or loss of CO2 inside the chamber. One complete cycle including two chamber measurements last 70 minutes. The buoy can be deployed for more than 15 hours, and at wind speeds of up to 10 m/s. Floating chambers are known to overestimate fluxes due to the creation of additional turbulence at the water surface. We check that by measuring turbulence with two Acoustic Doppler Velocimeter, one directly underneath the center of the floating chamber (equipped with an inertial motion unit) and the other one positioned sideways to measure turbulence outside the perimeter of the buoy. To control the conditions below the floating chamber, a sensor which measures temperature, pressure and humidity was installed inside the chamber. ...
format Article in Journal/Newspaper
author Banko-Kubis, Hanne
Wurl, Oliver
Ribas-Ribas, Mariana
author_facet Banko-Kubis, Hanne
Wurl, Oliver
Ribas-Ribas, Mariana
author_sort Banko-Kubis, Hanne
title Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ...
title_short Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ...
title_full Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ...
title_fullStr Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ...
title_full_unstemmed Measurements of pCO2 and turbulence from an autonomous drifting buoy in July 2017 in the Norwegian fjords and adjacent North Atlantic waters during cruise HE491 ...
title_sort measurements of pco2 and turbulence from an autonomous drifting buoy in july 2017 in the norwegian fjords and adjacent north atlantic waters during cruise he491 ...
publisher PANGAEA
publishDate 2019
url https://dx.doi.org/10.1594/pangaea.900728
https://doi.pangaea.de/10.1594/PANGAEA.900728
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1038/s41598-019-42911-6
https://dx.doi.org/10.1016/j.oceano.2019.04.002
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.90072810.1038/s41598-019-42911-610.1016/j.oceano.2019.04.002
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