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author Krahmann, Gerd
Dilmahamod, Ahmad Fehmi
author_facet Krahmann, Gerd
Dilmahamod, Ahmad Fehmi
collection Datos científicos de ciencias marinas y ambientales
contents Temperature, salinity, and oxygen were obtained from a Seabird 911 plus CTD system equipped with two independently working sets of temperature–conductivity–oxygen. 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 Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_959720
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Temperature, salinity and oxygen measured on CTD water bottle samples and apparent oxygen utilization and relative precentage of South Atlantic Central Water (SACW) during METEOR cruise M160
Krahmann, Gerd
Dilmahamod, Ahmad Fehmi
apparent oxygen utilization; Cast number; CTD; CTD/Rosette; CTD-RO; Date/time end; Date/time start; DEPTH, water; Event label; LATITUDE; LONGITUDE; M160; M160_106-1; M160_132-1; M160_134-1; M160_136-1; M160_141-1; M160_149-1; M160_165-1; M160_168-1; M160_17-1; M160_175-1; M160_180-1; M160_184-1; M160_188-1; M160_194-1; M160_200-1; M160_21-1; M160_38-1; M160_40-1; M160_43-1; M160_63-1; M160_65-1; M160_67-1; M160_69-1; M160_73-1; M160_75-1; M160_84-1; M160_88-1; M160_94-1; M160_96-1; M160_98-1; Meteor (1986); North Atlantic Ocean; Oxygen; Oxygen, apparent utilization; REEBUS; Role of Eddies for the Carbon Pump in Coastal upwelling Areas; SACW; Salinity; Sample ID; Station label; Temperature; Temperature, water; Water mass
Temperature, salinity, and oxygen were obtained from a Seabird 911 plus CTD system equipped with two independently working sets of temperature–conductivity–oxygen. 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).
title Temperature, salinity and oxygen measured on CTD water bottle samples and apparent oxygen utilization and relative precentage of South Atlantic Central Water (SACW) during METEOR cruise M160
topic apparent oxygen utilization; Cast number; CTD; CTD/Rosette; CTD-RO; Date/time end; Date/time start; DEPTH, water; Event label; LATITUDE; LONGITUDE; M160; M160_106-1; M160_132-1; M160_134-1; M160_136-1; M160_141-1; M160_149-1; M160_165-1; M160_168-1; M160_17-1; M160_175-1; M160_180-1; M160_184-1; M160_188-1; M160_194-1; M160_200-1; M160_21-1; M160_38-1; M160_40-1; M160_43-1; M160_63-1; M160_65-1; M160_67-1; M160_69-1; M160_73-1; M160_75-1; M160_84-1; M160_88-1; M160_94-1; M160_96-1; M160_98-1; Meteor (1986); North Atlantic Ocean; Oxygen; Oxygen, apparent utilization; REEBUS; Role of Eddies for the Carbon Pump in Coastal upwelling Areas; SACW; Salinity; Sample ID; Station label; Temperature; Temperature, water; Water mass
url https://doi.org/10.1594/PANGAEA.959720