Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ...
This dataset includes calculated data over the epi-mesopelagic layer (0-800 m depth) of 26 stations with 14 of them inside or in the vicinity of a cyclonic eddy that formed off Mauritania along the ∼ 900 km zonal corridor between Mauritania and the Cabo Verde islands in the eastern Tropical North At...
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Online Access: | https://dx.doi.org/10.1594/pangaea.959741 https://doi.pangaea.de/10.1594/PANGAEA.959741 |
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ftdatacite:10.1594/pangaea.959741 2023-11-05T03:43:59+01:00 Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ... Dilmahamod, Ahmad Fehmi 2023 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.959741 https://doi.pangaea.de/10.1594/PANGAEA.959741 en eng PANGAEA https://dx.doi.org/10.1029/2023jc019821 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 apparent oxygen utilization SACW Event label Station label DATE/TIME LATITUDE LONGITUDE DEPTH, water Water mass Oxygen, apparent utilization CTD/Rosette M156 Meteor 1986 Role of Eddies for the Carbon Pump in Coastal upwelling Areas REEBUS Dataset dataset 2023 ftdatacite https://doi.org/10.1594/pangaea.95974110.1029/2023jc019821 2023-10-09T10:48:52Z This dataset includes calculated data over the epi-mesopelagic layer (0-800 m depth) of 26 stations with 14 of them inside or in the vicinity of a cyclonic eddy that formed off Mauritania along the ∼ 900 km zonal corridor between Mauritania and the Cabo Verde islands in the eastern Tropical North Atlantic during the M156 cruise on the RV Meteor from July 3rd to August 1st 2019. The apparent oxygen utilization was calculated as the difference between saturation concentrations of O2 and measured O2 concentrations: AOU= [O2sat ({*}{*}θ{*}{*}, S)] − [O2], with S = salinity and θ = potential temperature (Redfield, 1942; Redfield et al., 1963; Pytkowicz, 1971). The saturated oxygen (O2sat) was computed using measured temperature and salinity following 212 Garcia and Gordon (1992). Relative percentage of South Atlantic Central Water was determined as in Klenz et al., (2018). ... Dataset North Atlantic DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
apparent oxygen utilization SACW Event label Station label DATE/TIME LATITUDE LONGITUDE DEPTH, water Water mass Oxygen, apparent utilization CTD/Rosette M156 Meteor 1986 Role of Eddies for the Carbon Pump in Coastal upwelling Areas REEBUS |
spellingShingle |
apparent oxygen utilization SACW Event label Station label DATE/TIME LATITUDE LONGITUDE DEPTH, water Water mass Oxygen, apparent utilization CTD/Rosette M156 Meteor 1986 Role of Eddies for the Carbon Pump in Coastal upwelling Areas REEBUS Dilmahamod, Ahmad Fehmi Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ... |
topic_facet |
apparent oxygen utilization SACW Event label Station label DATE/TIME LATITUDE LONGITUDE DEPTH, water Water mass Oxygen, apparent utilization CTD/Rosette M156 Meteor 1986 Role of Eddies for the Carbon Pump in Coastal upwelling Areas REEBUS |
description |
This dataset includes calculated data over the epi-mesopelagic layer (0-800 m depth) of 26 stations with 14 of them inside or in the vicinity of a cyclonic eddy that formed off Mauritania along the ∼ 900 km zonal corridor between Mauritania and the Cabo Verde islands in the eastern Tropical North Atlantic during the M156 cruise on the RV Meteor from July 3rd to August 1st 2019. The apparent oxygen utilization was calculated as the difference between saturation concentrations of O2 and measured O2 concentrations: AOU= [O2sat ({*}{*}θ{*}{*}, S)] − [O2], with S = salinity and θ = potential temperature (Redfield, 1942; Redfield et al., 1963; Pytkowicz, 1971). The saturated oxygen (O2sat) was computed using measured temperature and salinity following 212 Garcia and Gordon (1992). Relative percentage of South Atlantic Central Water was determined as in Klenz et al., (2018). ... |
format |
Dataset |
author |
Dilmahamod, Ahmad Fehmi |
author_facet |
Dilmahamod, Ahmad Fehmi |
author_sort |
Dilmahamod, Ahmad Fehmi |
title |
Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ... |
title_short |
Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ... |
title_full |
Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ... |
title_fullStr |
Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ... |
title_full_unstemmed |
Apparent oxygen utilization and relative percentage of South Atlantic Central Water (SACW) during METEOR cruise M156 ... |
title_sort |
apparent oxygen utilization and relative percentage of south atlantic central water (sacw) during meteor cruise m156 ... |
publisher |
PANGAEA |
publishDate |
2023 |
url |
https://dx.doi.org/10.1594/pangaea.959741 https://doi.pangaea.de/10.1594/PANGAEA.959741 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://dx.doi.org/10.1029/2023jc019821 |
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.95974110.1029/2023jc019821 |
_version_ |
1781702941310189568 |