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  • PANGAEA  (14)
  • AGU (American Geophysical Union)  (3)
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  • 1
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    AGU (American Geophysical Union)
    In:  Geophysical Research Letters, 24 . pp. 1763-1766.
    Publication Date: 2018-02-13
    Description: The partial pressure of CO2 (pCO2) was measured during the 1995 South-West Monsoon in the Arabian Sea. The Arabian Sea was characterized throughout by a moderate supersaturation of 12–30 µatm. The stable atmospheric pCO2 level was around 345 µatm. An extreme supersaturation was found in areas of coastal upwelling off the Omani coast with pCO2 peak values in surface waters of 750 µatm. Such two-fold saturation (218%) is rarely found elsewhere in open ocean environments. We also encountered cold upwelled water 300 nm off the Omani coast in the region of Ekman pumping, which was also characterized by a strongly elevated seawater pCO2 of up to 525 µatm. Due to the strong monsoonal wind forcing the Arabian Sea as a whole and the areas of upwelling in particular represent a significant source of atmospheric CO2 with flux densities from around 2 mmol m−2 d−1 in the open ocean to 119 mmol m−2 d−1 in coastal upwelling. Local air masses passing the area of coastal upwelling showed increasing CO2 concentrations, which are consistent with such strong emissions.
    Type: Article , PeerReviewed
    Format: text
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  • 2
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    AGU (American Geophysical Union)
    In:  Journal of Geophysical Research: Oceans, 103 (C9). pp. 18681-18689.
    Publication Date: 2018-04-30
    Description: The penetration of anthropogenic or “excess” CO2 into the North Atlantic Ocean was studied along WOCE‐WHP section A2 from 49°N/11°W to 43°N/49°W using hydrographic data obtained during the METEOR cruise 30–2 in October/November 1994. A backcalculation technique based on measurements of temperature, salinity, oxygen, alkalinity, and total dissolved inorganic carbon was applied to identify the excess CO2. Everywhere along the transect surface water contained almost its full component of anthropogenic CO2 ( ∼62 μmol kg−1). Furthermore, anthropogenic CO2 has penetrated through the entire water column in the western basin of the North Atlantic Ocean. Even in the deepest waters (5000 m) of the western basin a mean value of 10.4 μmol kg−1 excess CO2 was calculated. The maximum penetration depth of excess CO2 in the eastern basin of the North Atlantic Ocean was ∼3500 m with values falling below 5 μmol kg−1 in greater depths. These results compare well with distributions of carbontetrachloride. They are also in agreement with the current understanding of the role of the “global ocean conveyor belt” for the uptake of anthropogenic CO2 into the deep ocean.
    Type: Article , PeerReviewed
    Format: text
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  • 3
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    AGU (American Geophysical Union)
    In:  Geophysical Research Letters, 26 . pp. 2065-2068.
    Publication Date: 2018-02-13
    Description: We compare estimates of the anthropogenic CO2 content of seawater samples from the subpolar North Atlantic Ocean calculated on the basis of a back-calculation technique with measurements of the chlorofluorocarbon CFC-11. Estimated anthropogenic CO2 concentrations are in the range 10–80 µmol kg-1, while CFC-11 concentrations cover the full range from below detection limit to 〉 5 pmol kg-1 in waters at atmospheric equilibrium. The majority of the data points show a linear correlation between anthropogenic CO2 concentrations and CFC-11 saturation, which can only be explained by the strongly advective nature of the North Atlantic Ocean. Only deep eastern basin samples deviate from this general observation in that they show still significant concentrations of anthropogenic CO2 where CFC-11 is no longer detectable. In order to remove the influence of the Revelle factor reflected in the anthropogenic CO2 concentrations we have calculated 'excess' pCO2, showing an even tighter linear correlation with atmospheric equilibrium concentrations of CFC-11.
    Type: Article , PeerReviewed
    Format: text
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  • 4
    Publication Date: 2023-05-12
    Keywords: BI-1; Calculated; Carbon, organic, flux; DEPTH, water; Event label; FS-1; FS-3; FS-4; GB-2; Global Environmental Change: The Northern North Atlantic; Latitude of event; LB-1; Longitude of event; NA-1; NB1; Quaternary Environment of the Eurasian North; QUEEN; SFB313; SP-2_trap; Trap; TRAP; VP-2/3/4
    Type: Dataset
    Format: text/tab-separated-values, 10 data points
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  • 5
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    PANGAEA
    Publication Date: 2024-02-02
    Keywords: 06MT39_4; Carbon dioxide in the Atlantic Ocean; CARINA; CT; DATE/TIME; DEPTH, water; Fugacity of carbon dioxide (air, 100% humidity); Fugacity of carbon dioxide in seawater; LATITUDE; LONGITUDE; M39/4; M39/4-track; Meteor (1986); NDIR-based seawater-air equilibration technique; North Atlantic; Pressure, atmospheric; Salinity; Ship based meteorological sensor; Thermosalinograph; TSG; Underway cruise track measurements; Volume fraction of carbon dioxide in dry air
    Type: Dataset
    Format: text/tab-separated-values, 122682 data points
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  • 6
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    PANGAEA
    Publication Date: 2024-02-02
    Keywords: 06MT39_4; Carbon dioxide in the Atlantic Ocean; CARINA; CT; DATE/TIME; DEPTH, water; Fugacity of carbon dioxide (air, 100% humidity); Fugacity of carbon dioxide in seawater; LATITUDE; LONGITUDE; M39/4; M39/4-track; Meteor (1986); NDIR-based seawater-air equilibration technique; North Atlantic; Pressure, atmospheric; Salinity; Ship based meteorological sensor; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements; Volume fraction of carbon dioxide in dry air
    Type: Dataset
    Format: text/tab-separated-values, 163278 data points
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  • 7
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    PANGAEA
    In:  Supplement to: Körtzinger, Arne; Koeve, Wolfgang; Kähler, W; Mintrop, Ludger J (2001): C:N ratios in the mixed layer during the productive season in the northeast Atlantic Ocean. Deep Sea Research Part I: Oceanographic Research Papers, 48(3), 661-688, https://doi.org/10.1016/S0967-0637(00)00051-0
    Publication Date: 2024-06-26
    Description: Redfield stoichiometry has proved a robust paradigm for the understanding of biological production and export in the ocean on a long-term and a large-scale basis. However, deviations of carbon and nitrogen uptake ratios from the Redfield ratio have been reported. A comprehensive data set including all carbon and nitrogen pools relevant to biological production in the surface ocean (DIC, DIN, DOC, DON, POC, PON) was used to calculate seasonal new production based on carbon and nitrogen uptake in summer along 20°W in the northeast Atlantic Ocean. The 20°W transect between 30 and 60°N covers different trophic states and seasonal stages of the productive surface layer, including early bloom, bloom, post-bloom and non-bloom situations. The spatial pattern has elements of a seasonal progression. We also calculated exported production, i.e., that part of seasonal new production not accumulated in particulate and dissolved pools, again separately for carbon and nitrogen. The pairs of estimates of 'seasonal new production' and 'exported production' allowed us to calculate the C : N ratios of these quantities. While suspended particulate matter in the mixed layer largely conforms to Redfield stoichiometry, marked deviations were observed in carbon and nitrogen uptake and export with progressing season or nutrient depletion. The spring system was characterized by nitrogen overconsumption and the oligotrophic summer system by a marked carbon overconsumption. The C : N ratios of seasonal new as well as exported production increase from early bloom values of 5-6 to values of 10-16 in the post-bloom/oligotrophic system. The summertime accumulation of nitrogen-poor dissolved organic matter can explain only part of this shift.
    Keywords: Carbon, organic, particulate; Carbon, organic, total; Carbon, organic, total, standard deviation; DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; M36/2; M36/2_Sn-1; M36/2_Sn-10; M36/2_Sn-11; M36/2_Sn-12; M36/2_Sn-13; M36/2_Sn-14; M36/2_Sn-15; M36/2_Sn-16; M36/2_Sn-17; M36/2_Sn-18; M36/2_Sn-19; M36/2_Sn-2; M36/2_Sn-20; M36/2_Sn-21; M36/2_Sn-22; M36/2_Sn-23; M36/2_Sn-24; M36/2_Sn-25; M36/2_Sn-26; M36/2_Sn-27; M36/2_Sn-28; M36/2_Sn-29; M36/2_Sn-3; M36/2_Sn-30; M36/2_Sn-31; M36/2_Sn-32; M36/2_Sn-33; M36/2_Sn-34; M36/2_Sn-35; M36/2_Sn-36; M36/2_Sn-37; M36/2_Sn-38; M36/2_Sn-39; M36/2_Sn-4; M36/2_Sn-40; M36/2_Sn-41; M36/2_Sn-42; M36/2_Sn-43; M36/2_Sn-44; M36/2_Sn-45; M36/2_Sn-46; M36/2_Sn-47; M36/2_Sn-48; M36/2_Sn-5; M36/2_Sn-6; M36/2_Sn-7; M36/2_Sn-8; M36/2_Sn-9; Meteor (1986); Nitrogen, inorganic, dissolved; Nitrogen, organic, particulate; Nitrogen, organic+inorganic, particulate+dissolved; Nitrogen, standard deviation; North Atlantic; SNORKEL; Snorkel with pump
    Type: Dataset
    Format: text/tab-separated-values, 306 data points
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  • 8
    Publication Date: 2024-06-26
    Keywords: Alkalinity, potentiometric; Alkalinity, total; Carbon, inorganic, dissolved; Continuous Flow Automated Analysis (Gordon et al., 1993, WOCE Tech Rpt 93-1); Coulometric titration (Knap et al., 1996, IOC Manuals and Guides 29, UNESCO); CTD, Neil Brown, Mark III B; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; M36/2; M36/2-CTD-178_002; M36/2-CTD-178_003; M36/2-CTD-179_009; M36/2-CTD-179_010; M36/2-CTD-180_011; M36/2-CTD-180_012; M36/2-CTD-181_013; M36/2-CTD-181_014; M36/2-CTD-183_016; M36/2-CTD-183_017; M36/2-CTD-184_018; M36/2-CTD-184_019; M36/2-CTD-186_020; M36/2-CTD-186_021; M36/2-CTD-188_028; M36/2-CTD-188_029; M36/2-CTD-189_030; M36/2-CTD-189_031; M36/2-CTD-190_032; M36/2-CTD-190_033; M36/2-CTD-191_036; M36/2-CTD-193_038; M36/2-CTD-193_039; M36/2-CTD-194_040; M36/2-CTD-194_041; met036_2_003; Meteor (1986); Nitrate; Nitrite; Oxygen; Phosphate; Salinity; Silicate; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 3639 data points
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  • 9
    Publication Date: 2024-06-26
    Keywords: Carbon dioxide in the Atlantic Ocean; CARINA; CT; DATE/TIME; DEPTH, water; Fugacity of carbon dioxide (air, 100% humidity); Fugacity of carbon dioxide in seawater; JGOFS; Joint Global Ocean Flux Study; LATITUDE; LONGITUDE; M36/2; M36/2-track; Meteor (1986); NDIR-based seawater-air equilibration technique; North Atlantic; Pressure, atmospheric; Salinity; Ship based meteorological sensor; Temperature, water; Thermosalinograph; TSG; Underway cruise track measurements; Volume fraction of carbon dioxide in dry air; Wind direction; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 157677 data points
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  • 10
    Publication Date: 2024-06-28
    Keywords: 001; 002; 003; 004; 005; 006; 007; 008; 009; 010; 011; 012; 013; 014; 015; 016; 017; 018; 019; 020; 021; 022; 023; 024; 025; 026; 027; 028; 029; 030; 031; 032; 033; 034; 035; 036; 038; 039; 040; 041; 042; 044; 045; 046; 047; 048; 049; 050; 051; 052; 053; 054; 055; 056; 057; 058; 059; 060; 061; 062; 063; 064; 065; 066; 067; 068; 069; 070; 071; 072; 073; 074; 075; 076; 077; 079; 080; 081; Colorometric autoanalysis (unfiltered); Date/Time of event; DEPTH, water; Event label; GPUMP; JGOFS; Joint Global Ocean Flux Study; LATITUDE; LONGITUDE; Nitrate and Nitrite; Nitrite; Ocean Margin Exchange Project; OMEX; Phosphate; POS211; POS211_001; POS211_002; POS211_003; POS211_004; POS211_005; POS211_006; POS211_007; POS211_008; POS211_009; POS211_010; POS211_011; POS211_012; POS211_013; POS211_014; POS211_015; POS211_016; POS211_017; POS211_018; POS211_019; POS211_020; POS211_021; POS211_022; POS211_023; POS211_024; POS211_025; POS211_026; POS211_027; POS211_028; POS211_029; POS211_030; POS211_031; POS211_032; POS211_033; POS211_034; POS211_035; POS211_036; POS211_038; POS211_039; POS211_040; POS211_041; POS211_042; POS211_044; POS211_045; POS211_046; POS211_047; POS211_048; POS211_049; POS211_050; POS211_051; POS211_052; POS211_053; POS211_054; POS211_055; POS211_056; POS211_057; POS211_058; POS211_059; POS211_060; POS211_061; POS211_062; POS211_063; POS211_064; POS211_065; POS211_066; POS211_067; POS211_068; POS211_069; POS211_070; POS211_071; POS211_072; POS211_073; POS211_074; POS211_075; POS211_076; POS211_077; POS211_079; POS211_080; POS211_081; Poseidon; Ships non-toxic pump; Silicate
    Type: Dataset
    Format: text/tab-separated-values, 312 data points
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