Physical oceanography during METEOR cruise M91

DOI

Low Oxygen values are likely too high by 1 to 2 µmol/kg, higher values are ok. Near surface S values are problematic because of biology. A few negative oxygen values appear to be caused by an overshoot of Seabirds oxygen hysteresis correction in extremely strong vertical oxygen gradients. PAR with BadValue or NaN might need replacement by 0Fluorescence and Turbidity data still contain deck offsets. Use with caution.nc_uncertainty_p = 2.000000nc_uncertainty_t = 0.002000nc_uncertainty_s = 0.002000nc_uncertainty_o = 1.000000

Identifier
DOI https://doi.org/10.1594/PANGAEA.858090
Related Identifier https://doi.org/10.1594/PANGAEA.902689
Related Identifier https://doi.org/10.2312/cr_m91
Related Identifier https://doi.org/10.1594/PANGAEA.817221
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.858090
Provenance
Creator Krahmann, Gerd; Bange, Hermann Werner ORCID logo
Publisher PANGAEA
Publication Year 2016
Funding Reference German Research Foundation https://doi.org/10.13039/501100001659 Crossref Funder ID 27542298 https://gepris.dfg.de/gepris/projekt/27542298 Climate - Biogeochemistry Interactions in the Tropical Ocean
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 922683 data points
Discipline Biogeochemistry; Biospheric Sciences; Geosciences; Natural Sciences
Spatial Coverage (-82.000W, -16.156S, -75.332E, -5.000N); South Pacific Ocean
Temporal Coverage Begin 2012-12-02T13:05:39Z
Temporal Coverage End 2012-12-23T23:01:14Z