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  • 1
    Publication Date: 2023-10-28
    Description: NO was measured in the oxygen minimum zone (OMZ) of the eastern tropical South Pacific Ocean (ETSP) off Peru during the R/V Meteor cruise M93 in February/March 2013. NO was measured at nine stations by taking discrete water samples at selected water depths between the surface and 327 m with a pump-CTD system. NO concentrations were determined with a chemiluminescence NO analyser connected to a stripping unit. For details see Lutterbeck et al., Deep-Sea Res. II, 156, 148-154, 2018.
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; Date/Time of event; Depth, bottom/max; DEPTH, water; Error, relative; Event label; LATITUDE; LONGITUDE; M93; M93_347-3; M93_376-1; M93_378-1; M93_380-2; M93_391-10; M93_391-4; M93_399-4; M93_411-6; M93_441-2; M93_463-2; Meteor (1986); Nitric oxide; Nitric oxide, standard deviation; PCTD-RO; Pressure, water; PumpCTD/Rosette; Salinity; Sample code/label; SFB754; South Pacific Ocean; Station label; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 1016 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-10-28
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; CTD/Rosette; CTD 101; CTD 102; CTD 105; CTD 107; CTD 108; CTD 109; CTD 110; CTD 116; CTD 117; CTD 123; CTD 124; CTD 125; CTD 126; CTD 127; CTD 128; CTD 129; CTD 13; CTD 132; CTD 133; CTD 135; CTD 136; CTD 138; CTD 139; CTD 14; CTD 143; CTD 144; CTD 151; CTD 152; CTD 23; CTD 24; CTD 29; CTD 30; CTD 34; CTD 35; CTD 36; CTD 37; CTD 4; CTD 41; CTD 5; CTD 51; CTD 52; CTD 56; CTD 57; CTD 61; CTD 62; CTD 66; CTD 67; CTD 71; CTD 72; CTD-RO; DATE/TIME; DEPTH, water; Event label; Identification; LATITUDE; LONGITUDE; M90; M90_1555-1; M90_1555-2; M90_1563-1; M90_1563-2; M90_1572-1; M90_1572-2; M90_1577-1; M90_1577-2; M90_1581-1; M90_1581-2; M90_1582-1; M90_1583-1; M90_1586-1; M90_1596-1; M90_1596-2; M90_1600-1; M90_1600-2; M90_1604-1; M90_1604-2; M90_1608-1; M90_1608-2; M90_1612-1; M90_1612-2; M90_1639-1; M90_1639-2; M90_1642-1; M90_1644-1; M90_1645-1; M90_1646-1; M90_1646-2; M90_1652-1; M90_1652-2; M90_1657-1; M90_1658-1; M90_1659-1; M90_1659-2; M90_1660-1; M90_1661-1; M90_1661-2; M90_1664-1; M90_1664-2; M90_1666-1; M90_1666-2; M90_1668-1; M90_1668-2; M90_1672-1; M90_1673-1; M90_1679-1; M90_1679-2; Meteor (1986); Nitrous oxide, dissolved; Sample code/label; SFB754
    Type: Dataset
    Format: text/tab-separated-values, 4752 data points
    Location Call Number Limitation Availability
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  • 3
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    PANGAEA
    In:  GEOMAR - Helmholtz Centre for Ocean Research Kiel
    Publication Date: 2023-10-28
    Keywords: Bottle number; Climate - Biogeochemistry Interactions in the Tropical Ocean; CTD/Rosette; CTD001; CTD002; CTD003; CTD004; CTD005; CTD006; CTD008; CTD009; CTD010; CTD011; CTD012; CTD013; CTD014; CTD015; CTD016; CTD017; CTD018; CTD019; CTD020; CTD021; CTD022; CTD023; CTD024; CTD025; CTD026; CTD027; CTD028; CTD029; CTD030; CTD031; CTD032; CTD033; CTD034; CTD035; CTD036; CTD037; CTD038; CTD039; CTD040; CTD041; CTD042; CTD043; CTD044; CTD045; CTD046; CTD047; CTD048; CTD049; CTD050; CTD051; CTD052; CTD053; CTD054; CTD055; CTD056; CTD057; CTD058; CTD059; CTD060; CTD061; CTD062; CTD063-64; CTD065; CTD066; CTD067; CTD068; CTD069; CTD070; CTD071; CTD072; CTD073; CTD074; CTD075; CTD076; CTD077; CTD078; CTD079; CTD080; CTD081; CTD082; CTD083; CTD086; CTD087; CTD088; CTD089; CTD090; CTD091; CTD092; CTD093; CTD094; CTD095; CTD096; CTD097; CTD098; CTD101; CTD102; CTD103; CTD104; CTD105; CTD107; CTD109; CTD110; CTD111; CTD112; CTD113; CTD114; CTD115; CTD116; CTD117; CTD118; CTD119; CTD120; CTD121; CTD122; CTD123; CTD124; CTD125; CTD131; CTD132; CTD133; CTD134; CTD136; CTD137; CTD138; CTD139; CTD140; CTD141; CTD142; CTD143; CTD144; CTD145; CTD146; CTD147; CTD148; CTD149; CTD150; CTD151; CTD153; CTD154; CTD155; CTD156; CTD157; CTD158; CTD159; CTD160; CTD-RO; DATE/TIME; DEPTH, water; Event label; LATITUDE; LONGITUDE; M93; M93_290-1; M93_291-1; M93_292-1; M93_293-1; M93_295-1; M93_295-3; M93_298-1; M93_299-1; M93_300-1; M93_301-1; M93_302-1; M93_303-2; M93_304-1; M93_305-1; M93_306-1; M93_307-1; M93_308-1; M93_309-1; M93_310-1; M93_311-1; M93_312-1; M93_313-1; M93_314-1; M93_315-1; M93_316-1; M93_317-1; M93_318-2; M93_318-4; M93_318-6; M93_319-1; M93_320-1; M93_321-1; M93_322-1; M93_323-1; M93_324-1; M93_325-1; M93_326-1; M93_327-1; M93_328-1; M93_329-1; M93_330-1; M93_331-1; M93_332-1; M93_334-1; M93_335-1; M93_336-1; M93_337-1; M93_338-1; M93_339-1; M93_340-1; M93_341-1; M93_342-1; M93_343-1; M93_344-1; M93_345-1; M93_346-1; M93_347-2; M93_347-4; M93_347-6; M93_349-3; M93_350-1; M93_351-1; M93_354-1; M93_356-1; M93_357-1; M93_358-1; M93_359-2; M93_360-1; M93_361-2; M93_363-1; M93_364-1; M93_365-1; M93_366-1; M93_367-1; M93_368-1; M93_368-3; M93_369-1; M93_369-4; M93_376-2; M93_378-2; M93_380-3; M93_384-1; M93_384-2; M93_385-1; M93_386-1; M93_387-1; M93_388-1; M93_389-1; M93_390-1; M93_391-2; M93_391-5; M93_392-1; M93_393-1; M93_394-1; M93_399-5; M93_399-7; M93_404-1; M93_405-1; M93_406-1; M93_408-1; M93_411-2; M93_411-7; M93_411-9; M93_412-1; M93_413-1; M93_414-1; M93_415-1; M93_416-1; M93_417-1; M93_418-1; M93_419-1; M93_420-1; M93_421-1; M93_422-1; M93_423-1; M93_424-1; M93_425-1; M93_433-1; M93_434-1; M93_435-1; M93_436-1; M93_439-1; M93_441-3; M93_441-4; M93_441-5; M93_447-1; M93_448-1; M93_448-5; M93_456-1; M93_457-1; M93_458-1; M93_459-1; M93_460-1; M93_460-2; M93_461-1; M93_462-1; M93_463-1; M93_463-7; M93_465-1; M93_466-1; M93_467-1; M93_468-1; M93_469-1; M93_471-1; M93_471-2; Meteor (1986); Nitrous oxide; Oxygen; Salinity; SFB754; South Pacific Ocean; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 10354 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-08-12
    Description: Upward transport and/or mixing of trace gas-enriched subsurface waters fosters the exchange of nitrous oxide (N2O) and methane (CH4) with the atmosphere in the Eastern-South Atlantic (ESA). To date, it is, however, unclear whether this source is maintained by local production or advection of trace-gas enriched water masses. So, the meridional and zonal variability of N2O and CH4 in the ESA were investigated to constrain the contributions of the major regional water masses to the overall budget of N2O and CH4. The fieldwork took place during the cruises M99 (July 31st - August 23rd, 2013) and M120 (October 17th - November 18th, 2015) onboard the R/V METEOR, which encompassed close-coastal and open ocean regions off Angola and Namibia. To investigate the regional concentration gradients of N2O and CH4 and corresponding sea-air fluxes, seven hydrographic sections (six zonal transects and one alongshore transect) were conducted between ~10°S and 26°S. Concentrations of dissolved N2O and CH4 in surface waters were continuously measured by using the Mobile Equilibrator Sensor System. To evaluate, the oceanic-atmospheric trace gas exchange, the atmospheric N2O and CH4 in ambient air were measured at several sporadic locations, with an inlet installed at 35 m height. The data were quality controlled by comparing with the data generated by NOAA in the nearest atmospheric sampling station (23.58° S, 15.03°E, Station NMB (Gobabeb, Namibia)). Also, to better understand the underlying patterns of the trace gas in the ESA, the vertical profiles were investigated by measuring discrete samples of N2O using the dynamic headspace method on M99. N2O and CH4 concentrations were also measured using a purge and trap system during M120 expedition.
    Keywords: Eastern Boundary Upwelling Syetms; Enhancing Prediction of Tropical Atlantic Climate and its Impact; Methane; nitrous oxide; PREFACE; SACUS/SACUS-II; Southwest African Coastal Upwelling System and Benguela Niños; trace gases
    Type: Dataset
    Format: application/zip, 4 datasets
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-10-28
    Description: N2O production rates from ammonium, nitrite and nitrate and nitrate reduction rates and ammonium oxidation rates from the top 400 m water depth off the coast of Peru sampled from R/V Meteor during M138 in June 2017.
    Keywords: Ammonium; Ammonium, oxidation rate; Climate - Biogeochemistry Interactions in the Tropical Ocean; CTD/Rosette; CTD 013; CTD 018; CTD 036; CTD 044; CTD 063; CTD 069; CTD 076; CTD 085; CTD 099; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; ELEVATION; Event label; LATITUDE; LONGITUDE; M138; M138_882-11; M138_883-15; M138_892-3; M138_894-4; M138_904-7; M138_906-7; M138_907-7; M138_912-1; M138_917-3; Meteor (1986); Nitrate; Nitrate, reduction rate; Nitrate and Nitrite; Nitrite; Nitrous oxide production; OMZ; Oxygen; Phosphate; Ratio; Salinity; Sample code/label; SFB754; Silicate; Standard deviation; Standard error; Temperature, water; Yield
    Type: Dataset
    Format: text/tab-separated-values, 474 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2023-12-18
    Description: The data set comprises concentrations of dissolved N2O from seawater samples collected during the 36th Chinese Antarctic Research Expedition (36th CHINARE). The 36th CHINARE took place onboard the research vessel/icebreaker Xuelong 2 between the 3rd and 31st of January 2020 and focused on physical and biogeochemical surveys of the Ross Sea (Pacific sector of the Southern Ocean). Samples were collected by drawing water from 10 L Niskin bottles (installed on a standard CTD-Rosette) into brown borosilicate 20 mL vials, which were then sealed with rubber (butyl) stoppers and aluminium caps. Immediately after collection, samples were preserved by adding 0.05 mL of a saturated mercuric chloride solution. Samples were analyzed by means of a standard headspace method coupled to gas chromatography/electron capture detection. Details on the measurement equipment and data analysis can be found in Kock et al. (2016; see: www.biogeosciences.net/13/827/2016/).
    Keywords: Chinare36; Chinare36_A11-0-1; Chinare36_A11-0-10; Chinare36_A11-0-2; Chinare36_A11-0-3; Chinare36_A11-0-4; Chinare36_A11-0-5; Chinare36_A11-0-6; Chinare36_A11-0-7; Chinare36_A11-0-8; Chinare36_A11-0-9; Chinare36_A11-1-1; Chinare36_A11-1-10; Chinare36_A11-1-2; Chinare36_A11-1-3; Chinare36_A11-1-4; Chinare36_A11-1-5; Chinare36_A11-1-6; Chinare36_A11-1-7; Chinare36_A11-1-8; Chinare36_A11-1-9; Chinare36_A11-2-1; Chinare36_A11-2-10; Chinare36_A11-2-2; Chinare36_A11-2-3; Chinare36_A11-2-4; Chinare36_A11-2-5; Chinare36_A11-2-6; Chinare36_A11-2-7; Chinare36_A11-2-8; Chinare36_A11-2-9; Chinare36_A11-3-1; Chinare36_A11-3-10; Chinare36_A11-3-2; Chinare36_A11-3-3; Chinare36_A11-3-4; Chinare36_A11-3-5; Chinare36_A11-3-6; Chinare36_A11-3-7; Chinare36_A11-3-8; Chinare36_A11-4-1; Chinare36_A11-4-2; Chinare36_A11-4-3; Chinare36_A11-4-4; Chinare36_A11-4-6; Chinare36_A11-4-7; Chinare36_A11-4-8; Chinare36_A11-4-9; Chinare36_A3-10-1; Chinare36_A3-10-10; Chinare36_A3-10-11; Chinare36_A3-10-12; Chinare36_A3-10-13; Chinare36_A3-10-14; Chinare36_A3-10-2; Chinare36_A3-10-3; Chinare36_A3-10-4; Chinare36_A3-10-5; Chinare36_A3-10-6; Chinare36_A3-10-7; Chinare36_A3-10-8; Chinare36_A3-10-9; Chinare36_A3-5-1; Chinare36_A3-5-10; Chinare36_A3-5-11; Chinare36_A3-5-2; Chinare36_A3-5-3; Chinare36_A3-5-4; Chinare36_A3-5-5; Chinare36_A3-5-6; Chinare36_A3-5-7; Chinare36_A3-5-8; Chinare36_A3-5-9; Chinare36_A3-9-1; Chinare36_A3-9-10; Chinare36_A3-9-12; Chinare36_A3-9-13; Chinare36_A3-9-14; Chinare36_A3-9-2; Chinare36_A3-9-3; Chinare36_A3-9-4; Chinare36_A3-9-5; Chinare36_A3-9-6; Chinare36_A3-9-7; Chinare36_A3-9-8; Chinare36_A3-9-9; Chinare36_A4-3-1; Chinare36_A4-3-2; Chinare36_A4-3-3; Chinare36_A4-3-4; Chinare36_A4-3-6; Chinare36_A4-3-7; Chinare36_A4-3-8; Chinare36_A4-3-9; Chinare36_R1-1-1; Chinare36_R1-1-2; Chinare36_R1-1-3; Chinare36_R1-1-4; Chinare36_R1-1-6; Chinare36_R1-1-7; Chinare36_R1-1-8; Chinare36_R1-1-9; Chinare36_R1-2-1; Chinare36_R1-2-10; Chinare36_R1-2-2; Chinare36_R1-2-3; Chinare36_R1-2-4; Chinare36_R1-2-5; Chinare36_R1-2-6; Chinare36_R1-2-7; Chinare36_R1-2-8; Chinare36_R1-2-9; Chinare36_R1-3-1; Chinare36_R1-3-10; Chinare36_R1-3-2; Chinare36_R1-3-3; Chinare36_R1-3-4; Chinare36_R1-3-5; Chinare36_R1-3-6; Chinare36_R1-3-7; Chinare36_R1-3-8; Chinare36_R1-3-9; Chinare36_R1-4-1; Chinare36_R1-4-2; Chinare36_R1-4-3; Chinare36_R1-4-4; Chinare36_R1-4-5; Chinare36_R1-4-6; Chinare36_R1-4-7; Chinare36_R1-4-8; Chinare36_R1-4-9; Chinare36_R1-5-1; Chinare36_R1-5-2; Chinare36_R1-5-3; Chinare36_R1-5-5; Chinare36_R1-5-6; Chinare36_R1-5-8; Chinare36_R1-5-9; Chinare36_R1-6-1; Chinare36_R1-6-2; Chinare36_R1-6-3; Chinare36_R1-6-4; Chinare36_R1-6-5; Chinare36_R1-6-6; Chinare36_R1-6-7; Chinare36_R1-6-8; Chinare36_R1-6-9; Chinare36_R1-7-1; Chinare36_R1-7-2; Chinare36_R1-7-3; Chinare36_R1-7-4; Chinare36_R1-7-5; Chinare36_R1-7-6; Chinare36_R1-7-7; Chinare36_R1-7-8; Chinare36_R1-8-1; Chinare36_R1-8-2; Chinare36_R1-8-3; Chinare36_R1-8-4; Chinare36_R1-8-5; Chinare36_R1-8-6; Chinare36_R1-8-8; Chinare36_R1-8-9; Chinare36_RA1-0-1; Chinare36_RA1-0-10; Chinare36_RA1-0-11; Chinare36_RA1-0-12; Chinare36_RA1-0-13; Chinare36_RA1-0-2; Chinare36_RA1-0-3; Chinare36_RA1-0-4; Chinare36_RA1-0-5; Chinare36_RA1-0-6; Chinare36_RA1-0-7; Chinare36_RA1-0-8; Chinare36_RA1-0-9; Chinare36_RA1-1-1; Chinare36_RA1-1-10; Chinare36_RA1-1-11; Chinare36_RA1-1-12; Chinare36_RA1-1-13; Chinare36_RA1-1-2; Chinare36_RA1-1-3; Chinare36_RA1-1-4; Chinare36_RA1-1-5; Chinare36_RA1-1-6; Chinare36_RA1-1-7; Chinare36_RA1-1-8; Chinare36_RA1-1-9; Chinare36_RA1-2-1; Chinare36_RA1-2-10; Chinare36_RA1-2-11; Chinare36_RA1-2-12; Chinare36_RA1-2-13; Chinare36_RA1-2-2; Chinare36_RA1-2-3; Chinare36_RA1-2-4; Chinare36_RA1-2-5; Chinare36_RA1-2-6; Chinare36_RA1-2-7; Chinare36_RA1-2-8; Chinare36_RA1-2-9; Chinare36_RA1-3-1; Chinare36_RA1-3-10; Chinare36_RA1-3-11; Chinare36_RA1-3-12; Chinare36_RA1-3-13; Chinare36_RA1-3-2; Chinare36_RA1-3-3; Chinare36_RA1-3-4; Chinare36_RA1-3-5; Chinare36_RA1-3-6; Chinare36_RA1-3-7; Chinare36_RA1-3-8; Chinare36_RA1-3-9; Chinare36_RA1-4-3; Chinare36_RA1-4-4; Chinare36_RA1-4-5; Chinare36_RA1-4-6; Chinare36_RA1-4-7; Chinare36_RA1-4-8; Chinare36_RA1-4-9; Chinare36_RA1-5-1; Chinare36_RA1-5-10; Chinare36_RA1-5-11; Chinare36_RA1-5-12; Chinare36_RA1-5-13; Chinare36_RA1-5-14; Chinare36_RA1-5-2; Chinare36_RA1-5-3; Chinare36_RA1-5-4; Chinare36_RA1-5-5; Chinare36_RA1-5-6; Chinare36_RA1-5-7; Chinare36_RA1-5-8; Chinare36_RA1-5-9; Chinare36_RA1-6-1; Chinare36_RA1-6-10; Chinare36_RA1-6-11; Chinare36_RA1-6-12; Chinare36_RA1-6-13; Chinare36_RA1-6-14; Chinare36_RA1-6-2; Chinare36_RA1-6-3; Chinare36_RA1-6-4; Chinare36_RA1-6-5; Chinare36_RA1-6-6; Chinare36_RA1-6-7; Chinare36_RA1-6-8; Chinare36_RA1-6-9; Chinare36_RA1-7-1; Chinare36_RA1-7-10; Chinare36_RA1-7-11; Chinare36_RA1-7-12; Chinare36_RA1-7-13; Chinare36_RA1-7-14; Chinare36_RA1-7-3; Chinare36_RA1-7-4; Chinare36_RA1-7-5; Chinare36_RA1-7-6; Chinare36_RA1-7-7; Chinare36_RA1-7-8; Chinare36_RA1-7-9; Chinare36_RA2-1-1; Chinare36_RA2-1-10; Chinare36_RA2-1-11; Chinare36_RA2-1-2; Chinare36_RA2-1-3; Chinare36_RA2-1-4; Chinare36_RA2-1-5; Chinare36_RA2-1-6; Chinare36_RA2-1-7; Chinare36_RA2-1-8; Chinare36_RA2-1-9; Chinare36_RA2-2-1; Chinare36_RA2-2-10; Chinare36_RA2-2-11; Chinare36_RA2-2-12; Chinare36_RA2-2-13; Chinare36_RA2-2-2; Chinare36_RA2-2-3; Chinare36_RA2-2-4; Chinare36_RA2-2-5; Chinare36_RA2-2-6; Chinare36_RA2-2-7; Chinare36_RA2-2-8; Chinare36_RA2-2-9; Chinare36_RA2-3-1; Chinare36_RA2-3-10; Chinare36_RA2-3-11; Chinare36_RA2-3-2; Chinare36_RA2-3-3; Chinare36_RA2-3-4; Chinare36_RA2-3-5; Chinare36_RA2-3-6; Chinare36_RA2-3-7; Chinare36_RA2-3-8; Chinare36_RA2-3-9; Chinare36_RA2-5-1; Chinare36_RA2-5-10; Chinare36_RA2-5-11; Chinare36_RA2-5-12; Chinare36_RA2-5-13; Chinare36_RA2-5-14; Chinare36_RA2-5-2; Chinare36_RA2-5-3; Chinare36_RA2-5-4; Chinare36_RA2-5-5; Chinare36_RA2-5-6; Chinare36_RA2-5-7; Chinare36_RA2-5-8; Chinare36_RA2-5-9; Chinare36_RA2-6-1; Chinare36_RA2-6-10; Chinare36_RA2-6-11; Chinare36_RA2-6-12; Chinare36_RA2-6-13; Chinare36_RA2-6-14; Chinare36_RA2-6-2; Chinare36_RA2-6-3; Chinare36_RA2-6-4; Chinare36_RA2-6-5; Chinare36_RA2-6-6; Chinare36_RA2-6-7; Chinare36_RA2-6-8; Chinare36_RA2-6-9; Chinare36_RA2-7-1; Chinare36_RA2-7-10; Chinare36_RA2-7-11; Chinare36_RA2-7-12; Chinare36_RA2-7-13; Chinare36_RA2-7-14; Chinare36_RA2-7-2; Chinare36_RA2-7-3; Chinare36_RA2-7-4; Chinare36_RA2-7-5; Chinare36_RA2-7-6; Chinare36_RA2-7-7; Chinare36_RA2-7-8; Chinare36_RA2-7-9; Chinare36_RA3-2-1; Chinare36_RA3-2-2; Chinare36_RA3-2-3; Chinare36_RA3-2-4; Chinare36_RA3-2-5; Chinare36_RA3-2-6; Chinare36_RA3-2-7; Chinare36_RA3-2-8; Chinare36_RA3-2-9; Chinare36_RA3-3-1; Chinare36_RA3-3-10; Chinare36_RA3-3-11; Chinare36_RA3-3-12; Chinare36_RA3-3-2; Chinare36_RA3-3-3; Chinare36_RA3-3-4; Chinare36_RA3-3-5; Chinare36_RA3-3-6; Chinare36_RA3-3-7; Chinare36_RA3-3-8; Chinare36_RA3-3-9; Chinare36_RA3-4-1; Chinare36_RA3-4-10; Chinare36_RA3-4-11; Chinare36_RA3-4-2; Chinare36_RA3-4-3; Chinare36_RA3-4-4; Chinare36_RA3-4-5; Chinare36_RA3-4-6; Chinare36_RA3-4-7; Chinare36_RA3-4-8; Chinare36_RA3-4-9; Chinare36_RA3-5-1; Chinare36_RA3-5-10; Chinare36_RA3-5-11; Chinare36_RA3-5-12; Chinare36_RA3-5-13; Chinare36_RA3-5-2; Chinare36_RA3-5-3; Chinare36_RA3-5-4; Chinare36_RA3-5-5; Chinare36_RA3-5-6; Chinare36_RA3-5-7; Chinare36_RA3-5-8; Chinare36_RA3-5-9; Chinare36_RA3-6-1; Chinare36_RA3-6-10; Chinare36_RA3-6-11; Chinare36_RA3-6-12; Chinare36_RA3-6-13; Chinare36_RA3-6-2; Chinare36_RA3-6-3; Chinare36_RA3-6-4; Chinare36_RA3-6-5; Chinare36_RA3-6-6; Chinare36_RA3-6-7; Chinare36_RA3-6-8; Chinare36_RA3-6-9; Chinare36_RA3-7-10; Chinare36_RA3-7-11; Chinare36_RA3-7-12; Chinare36_RA3-7-13; Chinare36_RA3-7-14; Chinare36_RA3-7-2; Chinare36_RA3-7-3; Chinare36_RA3-7-4; Chinare36_RA3-7-5; Chinare36_RA3-7-6; Chinare36_RA3-7-7; Chinare36_RA3-7-8; Chinare36_RA3-7-9; DATE/TIME; Density, sigma, in situ; DEPTH, water; Event label; Greenhouse gases; LATITUDE; LONGITUDE; nitrous oxide; Nitrous oxide; Nitrous oxide, dissolved; Salinity; Southern Ocean; Temperature, water;
    Type: Dataset
    Format: text/tab-separated-values, 2460 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-02-02
    Description: The Benguela Upwelling System (BUS) is the most productive of all eastern boundary upwelling ecosystems and it hosts a well-developed oxygen minimum zone. As such, the BUS is a potential hotspot for production of N2O, a potent greenhouse gas derived from microbially driven decay of sinking organic matter. Yet, the extent at which near-surface waters emit N2O to the atmosphere in the BUS is highly uncertain. Here we present the first high-resolution surface measurements of N2O across the northern part of the BUS (nBUS).We found strong gradients with a threefold increase in N2O concentrations near the coast as compared with open ocean waters. Our observations show enhanced sea-to-air fluxes of N2O (up to 1.67 nmol m−2 s−1) in association with local upwelling cells. Based on our data we suggest that the nBUS can account for 13% of the total coastal upwelling source of N2O to the atmosphere
    Keywords: CT; DATE/TIME; DEPTH, water; Gas chromatography (unfiltered); LATITUDE; LONGITUDE; M99; M99-track; Meteor (1986); Nitrous oxide, dissolved; Nitrous oxide, dry-air mole fraction; Sea surface salinity; Sea surface temperature; SOPRAN; Southeast Atlantic; Surface Ocean Processes in the Anthropocene; Temperature at equilibration; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 92358 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2024-02-02
    Description: The Benguela Upwelling System (BUS) is the most productive of all eastern boundary upwelling ecosystems and it hosts a well-developed oxygen minimum zone. As such, the BUS is a potential hotspot for production of N2O, a potent greenhouse gas derived from microbially driven decay of sinking organic matter. Yet, the extent at which near-surface waters emit N2O to the atmosphere in the BUS is highly uncertain. Here we present the first high-resolution surface measurements of N2O across the northern part of the BUS (nBUS).We found strong gradients with a threefold increase in N2O concentrations near the coast as compared with open ocean waters. Our observations show enhanced sea-to-air fluxes of N2O (up to 1.67 nmol m−2 s−1) in association with local upwelling cells. Based on our data we suggest that the nBUS can account for 13% of the total coastal upwelling source of N2O to the atmosphere
    Keywords: ALTITUDE; Atlantic Ocean; BARO; Barometer; CT; DATE/TIME; Gas chromatography (unfiltered); INGOS; Integrated non-CO2 Greenhouse gas Observing System; LATITUDE; LONGITUDE; M98; M98-track; Meteor (1986); Nitrous oxide, dissolved; Nitrous oxide, dry-air mole fraction; Pressure, atmospheric; RACE SACUS; SACUS/SACUS-II; SOPRAN; Southwest African Coastal Upwelling System and Benguela Niños; Surface Ocean Processes in the Anthropocene; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 5614 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-02-02
    Description: The Benguela Upwelling System (BUS) is the most productive of all eastern boundary upwelling ecosystems and it hosts a well-developed oxygen minimum zone. As such, the BUS is a potential hotspot for production of N2O, a potent greenhouse gas derived from microbially driven decay of sinking organic matter. Yet, the extent at which near-surface waters emit N2O to the atmosphere in the BUS is highly uncertain. Here we present the first high-resolution surface measurements of N2O across the northern part of the BUS (nBUS).We found strong gradients with a threefold increase in N2O concentrations near the coast as compared with open ocean waters. Our observations show enhanced sea-to-air fluxes of N2O (up to 1.67 nmol m−2 s−1) in association with local upwelling cells. Based on our data we suggest that the nBUS can account for 13% of the total coastal upwelling source of N2O to the atmosphere
    Keywords: ALTITUDE; BARO; Barometer; Benguela Upwelling; CT; DATE/TIME; Gas chromatography (unfiltered); LATITUDE; LONGITUDE; M100/1; M100/1-track; Meteor (1986); Nitrous oxide, dissolved; Nitrous oxide, dry-air mole fraction; Pressure, atmospheric; SOPRAN; Surface Ocean Processes in the Anthropocene; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 127749 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-01-20
    Keywords: Climate - Biogeochemistry Interactions in the Tropical Ocean; CT; DATE/TIME; Fugacity of carbon dioxide (air, 100% humidity); Fugacity of carbon dioxide in seawater; LATITUDE; LONGITUDE; M93; M93-track; Meteor (1986); Salinity; SFB754; Southeast Pacific; Temperature, water; Underway cruise track measurements; Wind speed
    Type: Dataset
    Format: text/tab-separated-values, 6454 data points
    Location Call Number Limitation Availability
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