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Bibliographic Details
Main Authors: Podewski, Sigrid, Saure, G, Eppley, Richard W, Koeve, Wolfgang, Peinert, Rolf, Zeitzschel, Bernt
Format: Dataset Open Access
Language:en
Published: PANGAEA 1993
Subjects:
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
Online Access:https://doi.org/10.1594/PANGAEA.61809
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_version_ 1867168587954782208
author Podewski, Sigrid
Saure, G
Eppley, Richard W
Koeve, Wolfgang
Peinert, Rolf
Zeitzschel, Bernt
author_facet Podewski, Sigrid
Saure, G
Eppley, Richard W
Koeve, Wolfgang
Peinert, Rolf
Zeitzschel, Bernt
collection Datos científicos de ciencias marinas y ambientales
contents 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.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_61809
institution PANGAEA
language en
publishDate 1993
publisher PANGAEA
record_format pangaea
spellingShingle Physical oceanography during METEOR cruise M10/1
Podewski, Sigrid
Saure, G
Eppley, Richard W
Koeve, Wolfgang
Peinert, Rolf
Zeitzschel, Bernt
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
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.
title Physical oceanography during METEOR cruise M10/1
topic 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
url https://doi.org/10.1594/PANGAEA.61809