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  • 2010-2014  (18)
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Language
Years
Year
  • 1
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    Unknown
    IFM-GEOMAR, Kiel
    Publication Date: 2021-03-29
    Description: report
    Keywords: 551.4 ; 551.5 ; 910 ; 550 ; TYZ 100 ; UHF 300 ; UKB 200 ; Atlantischer Ozean {Meteorologie und Klimatologie} ; Wechselwirkungen zwischen Meer und Atmosphäre {Ozeanologie} ; Mittlerer Atlantik {Regionale Ozeanologie}
    Language: English
    Type: article , publishedVersion
    Format: application/pdf
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  • 2
    Publication Date: 2023-03-03
    Keywords: 06PO20050321; Alkalinity, total; Bottle number; Carbon, total; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Dibromomethane; Elevation of event; Event label; Freon-12 (dichlorodifluoromethane); Latitude of event; Longitude of event; Nitrate; Nitrite; Oxygen; Phosphate; POS320/1; POS320/1_36-1; POS320/1_36-2; POS320/1_37-1; POS320/1_38-1; POS320/1_40-1; POS320/1_41-1; POS320/1_42-1; POS320/1_43-1; POS320/1_44-1; POS320/1_45-1; POS320/1_46-1; POS320/1_46-2; POS320/1_47-1; POS320/1_48-1; POS320/1_48-2; POS320/1_49-1; POS320/1_50-1; POS320/1_51-1; POS320/1_52-1; POS320/1_52-2; POS320/1_53-1; POS320/1_54-1; POS320/1_55-1; POS320/1_55-2; POS320/1_56-1; POS320/1_57-1; POS320/1_57-2; POS320/1_58-1; POS320/1_58-2; POS320/1_59-1; POS320/1_60-1; POS320/1_61-1; POS320/1_61-2; POS320/1_62-1; POS320/1_63-1; POS320/1_64-1; POS320/1_65-1; POS320/1_65-2; POS320/1_66-1; POS320/1_66-2; POS320/1_67-1; POS320/1_68-1; POS320/1_68-2; Poseidon; Pressure, water; Salinity; Sample code/label; Silicate; Station label; Sulfur hexafluoride, SF6; Temperature, water; Tribromomethane; Tropical NE Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 5496 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Zindler, Cathleen; Bracher, Astrid; Marandino, Christa A; Taylor, Ben J; Torrecilla, Elena; Kock, Annette; Bange, Hermann Werner (2013): Sulphur compounds, methane, and phytoplankton: interactions along a north–south transit in the western Pacific Ocean. Biogeosciences, 10(5), 3297-3311, https://doi.org/10.5194/bg-10-3297-2013
    Publication Date: 2023-01-13
    Description: Here we present results of the first comprehensive study of sulphur compounds and methane in the oligotrophic tropical West Pacific Ocean. The concentrations of dimethylsuphide (DMS), dimethylsulphoniopropionate (DMSP), dimethylsulphoxide (DMSO), and methane (CH4), as well as various phytoplankton marker pigments in the surface ocean were measured along a north-south transit from Japan to Australia in October 2009. DMS (0.9 nmol/l), dissolved DMSP (DMSPd, 1.6 nmol/l) and particulate DMSP (DMSPp, 2 nmol/l) concentrations were generally low, while dissolved DMSO (DMSOd, 4.4 nmol/l) and particulate DMSO (DMSOp, 11.5 nmol/l) concentrations were comparably enhanced. Positive correlations were found between DMSO and DMSP as well as DMSP and DMSO with chlorophyll a, which suggests a similar source for both compounds. Similar phytoplankton groups were identified as being important for the DMSO and DMSP pool, thus, the same algae taxa might produce both DMSP and DMSO. In contrast, phytoplankton seemed to play only a minor role for the DMS distribution in the western Pacific Ocean. The observed DMSPp : DMSOp ratios were very low and seem to be characteristic of oligotrophic tropical waters representing the extreme endpoint of the global DMSPp : DMSOp ratio vs. SST relationship. It is most likely that nutrient limitation and oxidative stress in the tropical West Pacific Ocean triggered enhanced DMSO production leading to an accumulation of DMSO in the sea surface. Positive correlations between DMSPd and CH4, as well as between DMSO (particulate and total) and CH4, were found along the transit. We conclude that both DMSP and DMSO serve as substrates for methanogenic bacteria in the western Pacific Ocean.
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 4
    Publication Date: 2023-01-13
    Keywords: CT; DATE/TIME; ELEVATION; LATITUDE; LONGITUDE; Methane; Nitrous oxide, dissolved; Salinity; Sample code/label; SO202/2; SO202/2-track; Sonne; Temperature, water; TransBrom; Underway cruise track measurements; West Pacific
    Type: Dataset
    Format: text/tab-separated-values, 233 data points
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  • 5
    Publication Date: 2023-01-13
    Keywords: CT; DATE/TIME; DEPTH, water; Dimethyl sulfide, coefficient of variation; Dimethyl sulfide, dissolved; Dimethyl sulfide, standard deviation; Dimethylsulfoniopropionate; Dimethylsulfoniopropionate, dissolved; Dimethylsulfoniopropionate, dissolved, coefficient of variation; Dimethylsulfoniopropionate, dissolved, standard deviation; Dimethylsulfoniopropionate, particulate; Dimethylsulfoniopropionate, total, coefficient of variation; Dimethyl sulfoxide, dissolved; Dimethyl sulfoxide, dissolved, coefficient of variation; Dimethyl sulfoxide, dissolved, standard deviation; Dimethyl sulfoxide, particulate; Dimethyl sulfoxide, total; Dimethyl sulfoxide, total, coefficient of variation; Dimethyl sulfoxide, total, standard deviation; Dimethylsulphoniopropionate, total, standard deviation; LATITUDE; LONGITUDE; SO202/2; SO202/2-track; Sonne; TransBrom; Underway cruise track measurements; West Pacific
    Type: Dataset
    Format: text/tab-separated-values, 1856 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Kock, Annette; Schafstall, Jens; Dengler, Marcus; Brandt, Peter; Bange, Hermann Werner (2012): Sea-to-air and diapycnal nitrous oxide fluxes in the eastern tropical North Atlantic Ocean. Biogeosciences, 9(3), 957-964, https://doi.org/10.5194/bg-9-957-2012
    Publication Date: 2024-02-01
    Description: Sea-to-air and diapycnal fluxes of nitrous oxide (N2O) into the mixed layer were determined during three cruises to the upwelling region off Mauritania. Sea-to-air fluxes as well as diapycnal fluxes were elevated close to the shelf break, but elevated sea-to-air fluxes reached further offshore as a result of the offshore transport of upwelled water masses. To calculate a mixed layer budget for N2O we compared the regionally averaged sea-to-air and diapycnal fluxes and estimated the potential contribution of other processes, such as vertical advection and biological N2O production in the mixed layer. Using common parameterizations for the gas transfer velocity, the comparison of the average sea-toair and diapycnal N2O fluxes indicated that the mean sea-toair flux is about three to four times larger than the diapycnal flux. Neither vertical and horizontal advection nor biological production were found sufficient to close the mixed layer budget. Instead, the sea-to-air flux, calculated using a parameterization that takes into account the attenuating effect of surfactants on gas exchange, is in the same range as the diapycnal flux. From our observations we conclude that common parameterizations for the gas transfer velocity likely overestimate the air-sea gas exchange within highly productive upwelling zones.
    Keywords: SOPRAN; Surface Ocean Processes in the Anthropocene
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Schafstall, Jens; Dengler, Marcus; Brandt, Peter; Bange, Hermann Werner (2010): Tidal-induced mixing and diapycnal nutrient fluxes in the Mauritanian upwelling region. Journal of Geophysical Research, 115(C10), https://doi.org/10.1029/2009JC005940
    Publication Date: 2024-02-01
    Description: The Mauritanian coastal area is one of the most biologically productive upwelling regions in the world ocean. Shipboard observations carried out during maximum upwelling season and short-term moored observations are used to investigate diapycnal mixing processes and to quantify diapycnal fluxes of nutrients. The observations indicate strong tide-topography interactions that are favored by near-critical angles occurring on large parts of the continental slope. Moored velocity observations reveal the existence of highly nonlinear internal waves and bores and levels of internal wave spectra are strongly elevated near the buoyancy frequency. Dissipation rates of turbulent kinetic energy at the slope and shelf determined from microstructure measurements in the upper 200 m averages to ? = 5 × 10-8 W kg-1. Particularly elevated dissipation rates were found at the continental slope close to the shelf break, being enhanced by a factor of 100 to 1000 compared to dissipation rates farther offshore. Vertically integrated dissipation rates per unit volume are strongest at the upper continental slope reaching values of up to 30 mW m-2. A comparison of fine-scale parameterizations of turbulent dissipation rates for shelf regions and the open ocean to the measured dissipation rates indicates deficiencies in reproducing the observations. Diapycnal nitrate fluxes above the continental slope at the base of the mixed layer yielding a mean value of 12 × 10-2 µmol m-2 s-1 are amongst the largest published to date. However, they seem to only represent a minor contribution (10% to 25%) to the net community production in the upwelling region.
    Keywords: SOPRAN; Surface Ocean Processes in the Anthropocene
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 8
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    Unknown
    PANGAEA
    In:  GEOMAR - Helmholtz Centre for Ocean Research Kiel
    Publication Date: 2024-02-29
    Keywords: Bottle number; Calculated; Climate - Biogeochemistry Interactions in the Tropical Ocean; CTD; CTD/Rosette; CTD-001; CTD-002; CTD-003; CTD-004; CTD-005; CTD-006; CTD-007; CTD-008; CTD-009; CTD-010; CTD-011; CTD-012; CTD-013; CTD-014; CTD-015; CTD-016; CTD-017; CTD-018; CTD-019; CTD-020; CTD-021; CTD-022; CTD-023; CTD-024; CTD-025; CTD-026; CTD-027; CTD-028; CTD-029; CTD-030; CTD-031; CTD-032; CTD-033; CTD-034; CTD-035; CTD-036; CTD-037; CTD-038; CTD-039; CTD-040; CTD-041; CTD-042; CTD-043; CTD-044; CTD-045; CTD-046; CTD-047; CTD-048; CTD-049; CTD-050; CTD-051; CTD-052; CTD-053; CTD-054; CTD-055; CTD-056; CTD-057; CTD-058; CTD-059; CTD-060; CTD-061; CTD-062; CTD-063; CTD-064; CTD-065; CTD-066; CTD-067; CTD-068; CTD-069; CTD-070; CTD-071; CTD-072; CTD-073; CTD-074; CTD-075; CTD-076; CTD-077; CTD-078; CTD-079; CTD-080; CTD-081; CTD-082; CTD-083; CTD-084; CTD-085; CTD-086; CTD-087; CTD-088; CTD-089; CTD-090; CTD-091; CTD-092; CTD-093; CTD-094; CTD-095; CTD-096; CTD-097; CTD-RO; Date/Time of event; Density, sigma, in situ; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Latitude of event; Longitude of event; M91; M91_1712-1; M91_1713-1; M91_1713-3; M91_1714-1; M91_1715-1; M91_1715-3; M91_1716-1; M91_1717-1; M91_1718-1; M91_1719-1; M91_1720-1; M91_1721-1; M91_1721-3; M91_1722-1; M91_1723-1; M91_1724-1; M91_1724-3; M91_1725-1; M91_1725-3; M91_1726-1; M91_1727-1; M91_1727-3; M91_1728-1; M91_1729-1; M91_1730-1; M91_1731-1; M91_1732-1; M91_1733-1; M91_1733-13; M91_1733-6; M91_1734-1; M91_1735-1; M91_1736-1; M91_1736-3; M91_1737-1; M91_1737-3; M91_1738-1; M91_1739-1; M91_1739-3; M91_1740-1; M91_1741-1; M91_1742-1; M91_1743-1; M91_1744-1; M91_1745-1; M91_1746-1; M91_1747-1; M91_1748-1; M91_1749-1; M91_1750-1; M91_1751-1; M91_1751-3; M91_1752-1; M91_1752-12; M91_1752-4; M91_1752-8; M91_1753-1; M91_1754-1; M91_1755-2; M91_1755-4; M91_1756-1; M91_1757-1; M91_1758-1; M91_1759-1; M91_1760-1; M91_1761-1; M91_1762-2; M91_1763-1; M91_1764-1; M91_1764-12; M91_1764-3; M91_1764-8; M91_1765-1; M91_1766-1; M91_1766-3; M91_1767-1; M91_1767-2; M91_1768-1; M91_1768-3; M91_1769-1; M91_1770-2; M91_1770-4; M91_1771-1; M91_1772-1; M91_1773-2; M91_1773-3; M91_1774-1; M91_1774-3; M91_1775-1; M91_1775-3; M91_1776-1; M91_1776-3; M91_1777-1; M91_1777-12; M91_1777-4; M91_1777-7; M91_1778-1; Meteor (1986); Oxygen; Oxygen, Winkler (Culberson, 1991, WOCE Report 68/91); Pressure, water; Salinity; Salinometer, Guildline Instruments, 8400A Autosal; Sample ID; SFB754; SOPRAN; South Pacific Ocean; Surface Ocean Processes in the Anthropocene; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 19170 data points
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  • 9
    Publication Date: 2024-02-01
    Keywords: 23-10; CT; Eastern Tropical North Atlantic; LATITUDE; LONGITUDE; Nitrous oxide, dissolved; POS399/2; POS399/2-track; Poseidon; SOPRAN; Surface Ocean Processes in the Anthropocene; Time Stamp; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 5900 data points
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  • 10
    Publication Date: 2024-02-01
    Keywords: 23-10; amoA gene, copy number; Bottle number; CTD/Rosette; CTD10; CTD11; CTD12; CTD13; CTD14; CTD15; CTD16; CTD17; CTD18; CTD19; CTD2; CTD20; CTD21; CTD22; CTD23; CTD24; CTD25; CTD3; CTD4; CTD6; CTD7; CTD8; CTD9; CTD-RO; DATE/TIME; DEPTH, water; Event label; Micro structure probe; MSS; Nitrous oxide, coefficient of variation; Nitrous oxide, dissolved; Nitrous oxide, standard deviation; POS399/2; POS399/2_307-10; POS399/2_307-3; POS399/2_307-6; POS399/2_307-7; POS399/2_308-13; POS399/2_308-14; POS399/2_309-17; POS399/2_310-18; POS399/2_311-19; POS399/2_311-21; POS399/2_311-23; POS399/2_312-25; POS399/2_313-27; POS399/2_314-28; POS399/2_315-29; POS399/2_316-31; POS399/2_316-34; POS399/2_317-36; POS399/2_317-38; POS399/2_318-41; POS399/2_319-43; POS399/2_319-44; POS399/3; POS399/3_320-45; POS399/3_320-46; Poseidon; Sample ID; SOPRAN; Surface Ocean Processes in the Anthropocene
    Type: Dataset
    Format: text/tab-separated-values, 1090 data points
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