Physical oceanography during METEOR cruise M10/1, 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

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 s...

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Bibliographic Details
Main Authors: Podewski, Sigrid, Saure, G, Eppley, Richard W, Koeve, Wolfgang, Peinert, Rolf, Zeitzschel, Bernt
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 1993
Subjects:
CTD profile
Event label
Date/Time of event
Latitude of event
Longitude of event
Elevation of event
DEPTH, water
Pressure, water
Temperature, water
Salinity
Temperature, water, potential
Density, sigma-theta 0
CTD/Rosette
CTD, Neil Brown, Mark III B
Calculated from conductivity
Calculated
M10/1
Meteor 1986
Joint Global Ocean Flux Study JGOFS
North Atlantic Bloom Experiment, 1989-1991 NABE
Sigrid
North Atlantic
Northeast Atlantic
Online Access:https://dx.doi.org/10.1594/pangaea.61809
https://doi.pangaea.de/10.1594/PANGAEA.61809
Description
Summary: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. : see also the second part at doi:10.1594/PANGAEA.62022

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