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  • AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; Date/time end; Duration, number of days; Flux of total mass; Lithogenic, flux; Norwegian Sea; Sample code/label; Trap, sediment; TRAPS; VP-2_trap  (1)
  • Calculated; Calculated from conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; M10/1; M10/1-CTD-198_004; M10/1-CTD-199_005; M10/1-CTD-200_006; M10/1-CTD-201_007; M10/1-CTD-202_008; M10/1-CTD-203_009; M10/1-CTD-204_010; M10/1-CTD-205_011; M10/1-CTD-206_012; M10/1-CTD-207_013; M10/1-CTD-208_014; M10/1-CTD-209_015; M10/1-CTD-210_016; M10/1-CTD-211_017; M10/1-CTD-212_018; M10/1-CTD-213_019; M10/1-CTD-214_020; M10/1-CTD-215_021; M10/1-CTD-216_022; M10/1-CTD-217_023; M10/1-CTD-218_024; M10/1-CTD-219_025; M10/1-CTD-220_026; M10/1-CTD-221_027; M10/1-CTD-222_028; M10/1-CTD-223_029; M10/1-CTD-224_030; M10/1-CTD-225_031; M10/1-CTD-226_032; M10/1-CTD-227_033; M10/1-CTD-228_034; M10/1-CTD-229_035; M10/1-CTD-230_036; M10/1-CTD-231_037; M10/1-CTD-232_038; M10/1-CTD-233_039; M10/1-CTD-234_040; M10/1-CTD-235_041; M10/1-CTD-236_042; M10/1-CTD-237_043; M10/1-CTD-238_044; M10/1-CTD-239_045; M10/1-CTD-240_046; M10/1-CTD-241_047; M10/1-CTD-242_048; M10/1-CTD-244_049; M10/1-CTD-245_050; M10/1-CTD-246_051; M10/1-CTD-247_052; M10/1-CTD-249_053; M10/1-CTD-250_054; M10/1-CTD-251_055; M10/1-CTD-252_056; M10/1-CTD-253_057; M10/1-CTD-254_058; M10/1-CTD-255_059; M10/1-CTD-256_060; M10/1-CTD-256_061; M10/1-CTD-256_062; M10/1-CTD-257_063; M10/1-CTD-258_064; M10/1-CTD-259_065; M10/1-CTD-259_066; M10/1-CTD-260_067; M10/1-CTD-261_068; M10/1-CTD-262_069; M10/1-CTD-262_070; M10/1-CTD-262_071; M10/1-CTD-262_072; M10/1-CTD-262_073; M10/1-CTD-263_074; M10/1-CTD-264_075; M10/1-CTD-266_076; M10/1-CTD-267_077; M10/1-CTD-270_078; M10/1-CTD-273_079; M10/1-CTD-274_080; M10/1-CTD-277_081; M10/1-CTD-278_082; M10/1-CTD-279_083; M10/1-CTD-280_084; M10/1-CTD-282_085; M10/1-CTD-283_086; M10/1-CTD-284_087; M10/1-CTD-285_088; M10/1-CTD-286_089; M10/1-CTD-287_090; M10/1-CTD-288_091; M10/1-CTD-289_092; M10/1-CTD-290_093; M10/1-CTD-291_094; M10/1-CTD-291_095; M10/1-CTD-291_096; M10/1-CTD-291_097; M10/1-CTD-292_098; M10/1-CTD-293_099; M10/1-CTD-294_100; M10/1-CTD-295_101; M10/1-CTD-296_102; M10/1-CTD-297_103; M10/1-CTD-298_104; M10/1-CTD-299_105; M10/1-CTD-300_106; M10/1-CTD-301_107; M10/1-CTD-302_108; M10/1-CTD-303_109; M10/1-CTD-304_110; M10/1-CTD-305_111; M10/1-CTD-306_112; M10/1-CTD-307_113; M10/1-CTD-308_114; M10/1-CTD-309_115; M10/1-CTD-310_116; M10/1-CTD-311_117; M10/1-CTD-312_118; M10/1-CTD-313_119; M10/1-CTD-314_120; M10/1-CTD-315_121; M10/1-CTD-316_122; M10/1-CTD-317_123; M10/1-CTD-318_124; M10/1-CTD-319_125; M10/1-CTD-320_126; M10/1-CTD-321_127; M10/1-CTD-322_128; Meteor (1986); NABE; North Atlantic Bloom Experiment, 1989-1991; Pressure, water; Salinity; Temperature, water; Temperature, water, potential  (1)
  • Chlorophyll a; CTD/Rosette; CTD-RO; DEPTH, water; Global Environmental Change: The Northern North Atlantic; Lofoten; Phosphate; PO04_72; SFB313  (1)
Document type
Keywords
Publisher
Years
  • 1
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Bathmann, Ulrich; Peinert, Rolf; Noji, Thomas T; von Bodungen, Bodo (1990): Pelagic origin and fate of sedimenting particles in the Norwegian Sea. Progress in Oceanography, 24(1-4), 117-125, https://doi.org/10.1016/0079-6611(90)90024-V
    Publication Date: 2023-03-16
    Description: A 17 month record of vertical particle flux of dry weight, carbonate and organic carbon were 25.8, 9.4 and 2.4g/m**2/y, respectively. Parallel to trap deployments, pelagic system structure was recorded with high vertical and temporal resolution. Within a distinct seasonal cycle of vertical particle flux, zooplankton faecal pellets of various sizes, shapes and contents were collected by the traps in different proportions and quantities throughout the year (range: 0-4,500 10**3/m**2/d). The remains of different groups of organisms showed distinct seasonal variations in abundance. In early summer there was a small maximum in the diatom flux and this was followed by pulses of tinntinids, radiolarians, foraminiferans and pteropods between July and November. Food web interactions in the water column were important in controlling the quality and quantity of sinking materials. For example, changes in the population structure of dominant herbivores, the break-down of regenerating summer populations of microflagellates and protozooplankton and the collapse of a pteropod dominated community, each resulted in marked sedimentation pulses. These data from the Norwegian Sea indicate those mechanisms which either accelerate or counteract loss of material via sedimentation. These involve variations in the structure of the pelagic system and they operatè on long (e.g. annual plankton succession) and short (e.g. the end of new production, sporadic grazing of swarm feeders) time scales. Connecting investigation of the water column with a high resolution in time in parallel with drifting sediment trap deployments and shipboard experiments with the dominant zooplankters is a promising approach for giving a better understanding of both the origin and the fate of material sinking to the sea floor.
    Keywords: AWI_BioOce; Biological Oceanography @ AWI; DATE/TIME; Date/time end; Duration, number of days; Flux of total mass; Lithogenic, flux; Norwegian Sea; Sample code/label; Trap, sediment; TRAPS; VP-2_trap
    Type: Dataset
    Format: text/tab-separated-values, 55 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-01-14
    Keywords: Chlorophyll a; CTD/Rosette; CTD-RO; DEPTH, water; Global Environmental Change: The Northern North Atlantic; Lofoten; Phosphate; PO04_72; SFB313
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
    Location Call Number Limitation Availability
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Podewski, Sigrid; Saure, G; Eppley, Richard W; Koeve, Wolfgang; Peinert, Rolf; Zeitzschel, Bernt (1993): The nose: a characteristic inversion within the salinity maximum water in the tropical northeast Atlantic. Deep Sea Research Part II: Topical Studies in Oceanography, 40(1-2), 537-557, https://doi.org/10.1016/0967-0645(93)90031-H
    Publication Date: 2024-02-02
    Description: During leg 1 of Meteor cruise 10 in March/April 1989 at 18°N, 30°W, the high spatial and temporal resolution of hydrographic CTD-stations indicated that the study site was in a hydrographically complex region in the transition zone between the Canary Current and the North Equatorial Current at the southern boundary of the subtropical gyre. Strong variability was found within the upper 120 m due to interleavings of warmer and saltier subtropical salinity maximum water with colder and less saline upper thermocline water. The interleavings caused unexpected nose-like temperature, salinity, nitrate and oxygen profiles yet not described in the literature. A second variability source was found in the Central Water area, because the study area was situated in the vicinity of the Central Water Boundary dividing North and South Atlantic Central Water. Hydrographic analysis of the study shows that interpretations of biological and chemical data can only be done in conjunction with high resolution CTD-profiling.
    Keywords: Calculated; Calculated from conductivity; CTD, Neil Brown, Mark III B; CTD/Rosette; CTD profile; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; M10/1; M10/1-CTD-198_004; M10/1-CTD-199_005; M10/1-CTD-200_006; M10/1-CTD-201_007; M10/1-CTD-202_008; M10/1-CTD-203_009; M10/1-CTD-204_010; M10/1-CTD-205_011; M10/1-CTD-206_012; M10/1-CTD-207_013; M10/1-CTD-208_014; M10/1-CTD-209_015; M10/1-CTD-210_016; M10/1-CTD-211_017; M10/1-CTD-212_018; M10/1-CTD-213_019; M10/1-CTD-214_020; M10/1-CTD-215_021; M10/1-CTD-216_022; M10/1-CTD-217_023; M10/1-CTD-218_024; M10/1-CTD-219_025; M10/1-CTD-220_026; M10/1-CTD-221_027; M10/1-CTD-222_028; M10/1-CTD-223_029; M10/1-CTD-224_030; M10/1-CTD-225_031; M10/1-CTD-226_032; M10/1-CTD-227_033; M10/1-CTD-228_034; M10/1-CTD-229_035; M10/1-CTD-230_036; M10/1-CTD-231_037; M10/1-CTD-232_038; M10/1-CTD-233_039; M10/1-CTD-234_040; M10/1-CTD-235_041; M10/1-CTD-236_042; M10/1-CTD-237_043; M10/1-CTD-238_044; M10/1-CTD-239_045; M10/1-CTD-240_046; M10/1-CTD-241_047; M10/1-CTD-242_048; M10/1-CTD-244_049; M10/1-CTD-245_050; M10/1-CTD-246_051; M10/1-CTD-247_052; M10/1-CTD-249_053; M10/1-CTD-250_054; M10/1-CTD-251_055; M10/1-CTD-252_056; M10/1-CTD-253_057; M10/1-CTD-254_058; M10/1-CTD-255_059; M10/1-CTD-256_060; M10/1-CTD-256_061; M10/1-CTD-256_062; M10/1-CTD-257_063; M10/1-CTD-258_064; M10/1-CTD-259_065; M10/1-CTD-259_066; M10/1-CTD-260_067; M10/1-CTD-261_068; M10/1-CTD-262_069; M10/1-CTD-262_070; M10/1-CTD-262_071; M10/1-CTD-262_072; M10/1-CTD-262_073; M10/1-CTD-263_074; M10/1-CTD-264_075; M10/1-CTD-266_076; M10/1-CTD-267_077; M10/1-CTD-270_078; M10/1-CTD-273_079; M10/1-CTD-274_080; M10/1-CTD-277_081; M10/1-CTD-278_082; M10/1-CTD-279_083; M10/1-CTD-280_084; M10/1-CTD-282_085; M10/1-CTD-283_086; M10/1-CTD-284_087; M10/1-CTD-285_088; M10/1-CTD-286_089; M10/1-CTD-287_090; M10/1-CTD-288_091; M10/1-CTD-289_092; M10/1-CTD-290_093; M10/1-CTD-291_094; M10/1-CTD-291_095; M10/1-CTD-291_096; M10/1-CTD-291_097; M10/1-CTD-292_098; M10/1-CTD-293_099; M10/1-CTD-294_100; M10/1-CTD-295_101; M10/1-CTD-296_102; M10/1-CTD-297_103; M10/1-CTD-298_104; M10/1-CTD-299_105; M10/1-CTD-300_106; M10/1-CTD-301_107; M10/1-CTD-302_108; M10/1-CTD-303_109; M10/1-CTD-304_110; M10/1-CTD-305_111; M10/1-CTD-306_112; M10/1-CTD-307_113; M10/1-CTD-308_114; M10/1-CTD-309_115; M10/1-CTD-310_116; M10/1-CTD-311_117; M10/1-CTD-312_118; M10/1-CTD-313_119; M10/1-CTD-314_120; M10/1-CTD-315_121; M10/1-CTD-316_122; M10/1-CTD-317_123; M10/1-CTD-318_124; M10/1-CTD-319_125; M10/1-CTD-320_126; M10/1-CTD-321_127; M10/1-CTD-322_128; Meteor (1986); NABE; North Atlantic Bloom Experiment, 1989-1991; Pressure, water; Salinity; Temperature, water; Temperature, water, potential
    Type: Dataset
    Format: text/tab-separated-values, 263145 data points
    Location Call Number Limitation Availability
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