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  • PANGAEA  (40)
  • COPERNICUS GESELLSCHAFT MBH  (2)
  • Springer  (2)
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  • 11
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    PANGAEA
    In:  Supplement to: Brandt, Peter; Bange, Hermann Werner; Banyte, Donata; Dengler, Marcus; Didwischus, Sven-Helge; Fischer, Tim; Greatbatch, Richard J; Hahn, Johannes; Kanzow, Torsten; Karstensen, Johannes; Körtzinger, Arne; Krahmann, Gerd; Schmidtko, Sunke; Stramma, Lothar; Tanhua, Toste; Visbeck, Martin (2015): On the role of circulation and mixing in the ventilation of oxygen minimum zones with a focus on the eastern tropical North Atlantic. Biogeosciences, 12(2), 489-512, https://doi.org/10.5194/bg-12-489-2015
    Publication Date: 2024-02-01
    Description: Ocean observations carried out in the framework of the Collaborative Research Center 754 (SFB 754) "Climate-Biogeochemistry Interactions in the Tropical Ocean" are used to study (1) the structure of tropical oxygen minimum zones (OMZs), (2) the processes that contribute to the oxygen budget, and (3) long-term changes in the oxygen distribution. The OMZ of the eastern tropical North Atlantic (ETNA), located between the well-ventilated subtropical gyre and the equatorial oxygen maximum, is composed of a deep OMZ at about 400 m depth with its core region centred at about 20° W, 10° N and a shallow OMZ at about 100 m depth with lowest oxygen concentrations in proximity to the coastal upwelling region off Mauritania and Senegal. The oxygen budget of the deep OMZ is given by oxygen consumption mainly balanced by the oxygen supply due to meridional eddy fluxes (about 60%) and vertical mixing (about 20%, locally up to 30%). Advection by zonal jets is crucial for the establishment of the equatorial oxygen maximum. In the latitude range of the deep OMZ, it dominates the oxygen supply in the upper 300 to 400 m and generates the intermediate oxygen maximum between deep and shallow OMZs. Water mass ages from transient tracers indicate substantially older water masses in the core of the deep OMZ (about 120-180 years) compared to regions north and south of it. The deoxygenation of the ETNA OMZ during recent decades suggests a substantial imbalance in the oxygen budget: about 10% of the oxygen consumption during that period was not balanced by ventilation. Long-term oxygen observations show variability on interannual, decadal and multidecadal time scales that can partly be attributed to circulation changes. In comparison to the ETNA OMZ the eastern tropical South Pacific OMZ shows a similar structure including an equatorial oxygen maximum driven by zonal advection, but overall much lower oxygen concentrations approaching zero in extended regions. As the shape of the OMZs is set by ocean circulation, the widespread misrepresentation of the intermediate circulation in ocean circulation models substantially contributes to their oxygen bias, which might have significant impacts on predictions of future oxygen levels.
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; SFB754; SOPRAN; Surface Ocean Processes in the Anthropocene
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 12
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    PANGAEA
    In:  Supplement to: Fischer, Tim; Kock, Annette; Arévalo-Martínez, Damian L; Dengler, Marcus; Brandt, Peter; Bange, Hermann Werner (2019): Gas exchange estimates in the Peruvian upwelling regime biased by multi-day near-surface stratification. Biogeosciences, 16(11), 2307-2328, https://doi.org/10.5194/bg-16-2307-2019
    Publication Date: 2024-02-01
    Description: The coastal upwelling regime off Peru in December 2012 showed considerable vertical concentration gradients of dissolved nitrous oxide (N2O) across the top few meters of the ocean. The gradients were predominantly downward, i.e., concentrations decreased toward the surface. Ignoring these gradients causes a systematic error in regionally integrated gas exchange estimates, when using observed concentrations at several meters below the surface as input for bulk flux parameterizations – as is routinely practiced. Here we propose that multi-day near-surface stratification events are responsible for the observed near-surface N2O gradients, and that the gradients induce the strongest bias in gas exchange estimates at winds of about 3 to 6 m s−1. Glider hydrographic time series reveal that events of multi-day near-surface stratification are a common feature in the study region. In the same way as shorter events of near-surface stratification (e.g., the diurnal warm layer cycle), they preferentially exist under calm to moderate wind conditions, suppress turbulent mixing, and thus lead to isolation of the top layer from the waters below (surface trapping). Our observational data in combination with a simple gas-transfer model of the surface trapping mechanism show that multi-day near-surface stratification can produce near-surface N2O gradients comparable to observations. They further indicate that N2O gradients created by diurnal or shorter stratification cycles are weaker and do not substantially impact bulk emission estimates. Quantitatively, we estimate that the integrated bias for the entire Peruvian upwelling region in December 2012 represents an overestimation of the total N2O emission by about a third, if concentrations at 5 or 10 m depth are used as surrogate for bulk water N2O concentration. Locally, gradients exist which would lead to emission rates overestimated by a factor of two or more. As the Peruvian upwelling region is an N2O source of global importance, and other strong N2O source regions could tend to develop multi-day near-surface stratification as well, the bias resulting from multi-day near-surface stratification may also impact global oceanic N2O emission estimates.
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; SFB754; SOPRAN; Surface Ocean Processes in the Anthropocene
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 13
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    PANGAEA
    In:  IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University
    Publication Date: 2024-02-02
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; CT; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; LATITUDE; LONGITUDE; Maria S. Merian; MSM08/1; MSM08/1-track; SFB754; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 260518 data points
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  • 14
    Publication Date: 2024-02-02
    Keywords: Acoustic Doppler Current Profiling, vessel-mounted (VM-ADCP); Climate - Biogeochemistry Interactions in the Tropical Ocean; CT; File content; File format; File name; File size; M106; M106-track; Meteor (1986); SFB754; Underway cruise track measurements; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 15
    Publication Date: 2024-02-02
    Description: Upper-ocean velocities along the cruise track of Maria S. Merian cruise MSM106 were continuously collected by a vessel-mounted Teledyne RD Instruments 75 kHz Ocean Surveyor ADCP. The transducer was located at 6.0 m below the water line. The instrument was operated in three different configurations: 1) broadband mode with 4 m bins and a blanking distance of 2.0 m, with a total of 128 bins, 2) broadband mode with 8 m bins and a blanking distance of 4.0 m, with a total of 100 bins, 3) narrowband mode with 8 m bins and a blanking distance of 4.0 m, with a total of 100 bins. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). Heading, pitch and roll data from the ship's gyro platforms and the navigation data were used by the data acquisition software VmDas internally to convert ADCP velocities into earth coordinates. Accuracy of the ADCP velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data post-processing included water track calibration of the misalignment angle (configuration 1: 0.65° +/- 0.5915°, configuration 2: 0.78° +/- 0.5198°, configuration 3: 0.67° +/- 0.6996°) and scale factor (configuration1: 1.0075 +/- 0.0117, configuration 2: 1.0075 +/- 0.0087, configuration 3: 1.0007 +/- 0.0157) of the Ocean Surveyor signal. The average interval was set to 60 s.
    Keywords: Acoustic Doppler Current Profiler; ADCP; Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; LATITUDE; LONGITUDE; Maria S. Merian; MSM106; MSM106_0_Underway-2; MSM106_0_Underway-4; Pings, averaged to a double ensemble value; Quality flag, current velocity; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); South Atlantic Ocean; Vessel mounted Acoustic Doppler Current Profiler [75 kHz]; VMADCP-75; WASCAL
    Type: Dataset
    Format: text/tab-separated-values, 9650955 data points
    Location Call Number Expected Availability
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  • 16
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    PANGAEA
    In:  IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University
    Publication Date: 2024-02-02
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; CTD; CTD/Rosette; CTD1; CTD10; CTD11; CTD12; CTD13; CTD14; CTD15; CTD16; CTD17; CTD18; CTD19; CTD2; CTD20; CTD21; CTD22; CTD23; CTD24; CTD25; CTD26; CTD27; CTD28; CTD29; CTD3; CTD30; CTD31; CTD32; CTD33; CTD34; CTD35; CTD36; CTD37; CTD38; CTD39; CTD4; CTD40; CTD41; CTD42; CTD43; CTD44; CTD45; CTD46; CTD47; CTD48; CTD49; CTD5; CTD50; CTD51; CTD52; CTD53; CTD54; CTD55; CTD56; CTD57; CTD58; CTD59; CTD6; CTD60; CTD61; CTD62; CTD63; CTD64; CTD65; CTD66; CTD67; CTD68; CTD69; CTD7; CTD70; CTD71; CTD72; CTD73; CTD74; CTD75; CTD76; CTD77; CTD78; CTD79; CTD8; CTD80; CTD81; CTD82; CTD83; CTD84; CTD85; CTD86; CTD87; CTD88; CTD89; CTD9; CTD90; CTD91; CTD92; CTD93; CTD-RO; Date/Time of event; DEPTH, water; Event label; Fluorescence; Latitude of event; Longitude of event; Maria S. Merian; MSM18/3; MSM18/3_721-1; MSM18/3_722-1; MSM18/3_723-1; MSM18/3_724-1; MSM18/3_725-1; MSM18/3_726-1; MSM18/3_727-1; MSM18/3_728-1; MSM18/3_728-3; MSM18/3_728-4; MSM18/3_729-1; MSM18/3_730-1; MSM18/3_731-1; MSM18/3_732-1; MSM18/3_733-1; MSM18/3_734-2; MSM18/3_735-10; MSM18/3_735-12; MSM18/3_735-14; MSM18/3_735-2; MSM18/3_735-4; MSM18/3_735-6; MSM18/3_735-8; MSM18/3_736-1; MSM18/3_737-1; MSM18/3_738-1; MSM18/3_739-1; MSM18/3_740-1; MSM18/3_741-1; MSM18/3_742-1; MSM18/3_743-1; MSM18/3_743-3; MSM18/3_743-4; MSM18/3_745-1; MSM18/3_746-1; MSM18/3_747-1; MSM18/3_747-3; MSM18/3_747-4; MSM18/3_748-11; MSM18/3_748-2; MSM18/3_748-5; MSM18/3_748-7; MSM18/3_748-9; MSM18/3_750-1; MSM18/3_751-1; MSM18/3_752-1; MSM18/3_753-1; MSM18/3_754-2; MSM18/3_755-2; MSM18/3_756-1; MSM18/3_756-3; MSM18/3_756-4; MSM18/3_758-10; MSM18/3_758-12; MSM18/3_758-14; MSM18/3_758-2; MSM18/3_758-4; MSM18/3_758-6; MSM18/3_758-8; MSM18/3_759-1; MSM18/3_760-1; MSM18/3_764-1; MSM18/3_765-4; MSM18/3_766-2; MSM18/3_767-1; MSM18/3_768-1; MSM18/3_768-2; MSM18/3_768-4; MSM18/3_768-5; MSM18/3_769-10; MSM18/3_769-12; MSM18/3_769-14; MSM18/3_769-2; MSM18/3_769-4; MSM18/3_769-6; MSM18/3_769-8; MSM18/3_770-1; MSM18/3_771-1; MSM18/3_772-1; MSM18/3_773-1; MSM18/3_773-2; MSM18/3_773-4; MSM18/3_774-1; MSM18/3_775-10; MSM18/3_775-12; MSM18/3_775-14; MSM18/3_775-2; MSM18/3_775-4; MSM18/3_775-6; MSM18/3_775-8; MSM18/3_776-1; MSM18/3_778-1; MSM18/3_779-1; Oxygen; Pressure, water; Salinity; SFB754; SOPRAN; Surface Ocean Processes in the Anthropocene; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 301960 data points
    Location Call Number Expected Availability
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  • 17
    Publication Date: 2024-02-02
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; DATE/TIME; DEPTH, water; Event label; LATITUDE; LONGITUDE; Maria S. Merian; Micro structure probe; MSM10/1; MSM10/1-MSS10; MSM10/1-MSS11; MSM10/1-MSS12; MSM10/1-MSS13; MSM10/1-MSS14; MSM10/1-MSS15; MSM10/1-MSS16; MSM10/1-MSS17; MSM10/1-MSS18; MSM10/1-MSS19; MSM10/1-MSS20; MSM10/1-MSS21; MSM10/1-MSS3; MSM10/1-MSS4; MSM10/1-MSS5; MSM10/1-MSS6; MSM10/1-MSS7; MSM10/1-MSS8; MSM10/1-MSS9; MSS; Rate of turbulent kinetic energy dissipation; Salinity; SFB754; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 130181 data points
    Location Call Number Expected Availability
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  • 18
    Publication Date: 2024-02-02
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; CT; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; Event label; LATITUDE; LONGITUDE; M80/2; M80/2-track; Meteor (1986); SFB754; Tropical Atlantic; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 562966 data points
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  • 19
    Publication Date: 2024-02-02
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; CT; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; Event label; LATITUDE; LONGITUDE; Maria S. Merian; MSM10/1; MSM10/1-track; SFB754; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 815816 data points
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  • 20
    Publication Date: 2024-02-02
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; CT; Current velocity, east-west; Current velocity, north-south; DATE/TIME; DEPTH, water; Event label; LATITUDE; LONGITUDE; M83/1; M83/1-track; Meteor (1986); SFB754; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 490006 data points
    Location Call Number Expected Availability
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