Physical Oceanography in the tropical Atlantic oxygen minimum zone ...

The replenishment of consumed oxygen in the open ocean oxygen minimum zone (OMZ) off northwest Africa is accomplished by oxygen transport across and along density surfaces, i.e. diapycnal and isopycnal oxygen supply. Here the diapycnal oxygen supply is investigated using a large observational set of...

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Main Authors: Fischer, Tim, Banyte, Donata, Brandt, Peter, Dengler, Marcus, Krahmann, Gerd, Tanhua, Toste, Visbeck, Martin
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.819311
https://doi.pangaea.de/10.1594/PANGAEA.819311
id ftdatacite:10.1594/pangaea.819311
record_format openpolar
spelling ftdatacite:10.1594/pangaea.819311 2024-03-31T07:54:18+00:00 Physical Oceanography in the tropical Atlantic oxygen minimum zone ... Fischer, Tim Banyte, Donata Brandt, Peter Dengler, Marcus Krahmann, Gerd Tanhua, Toste Visbeck, Martin 2013 application/zip https://dx.doi.org/10.1594/pangaea.819311 https://doi.pangaea.de/10.1594/PANGAEA.819311 en eng PANGAEA https://dx.doi.org/10.5194/bg-10-5079-2013 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Climate - Biogeochemistry Interactions in the Tropical Ocean SFB754 Supplementary Publication Series of Datasets article Collection 2013 ftdatacite https://doi.org/10.1594/pangaea.81931110.5194/bg-10-5079-2013 2024-03-04T13:35:39Z The replenishment of consumed oxygen in the open ocean oxygen minimum zone (OMZ) off northwest Africa is accomplished by oxygen transport across and along density surfaces, i.e. diapycnal and isopycnal oxygen supply. Here the diapycnal oxygen supply is investigated using a large observational set of oxygen profiles and diapycnal mixing data from years 2008 to 2010. Diapycnal mixing is inferred from different sources: (i) a large-scale tracer release experiment, (ii) microstructure profiles, and (iii) shipboard?acoustic current measurements plus density profiles. From these measurements, the average diapycnal diffusivity in the studied depth interval from 150 to 500m is estimated to be 1×10**-5 m2 s**-1, with lower and upper 95% confidence limits of 0.8×10**-5 m2 s**-1 and 1.4×10**-5 m2 s**-1. Diapycnal diffusivity in this depth range is predominantly caused by turbulence, and shows no significant vertical gradient. Diapycnal mixing is found to contribute substantially to the oxygen supply of the OMZ. Within ... : Supplement to: Fischer, Tim; Banyte, Donata; Brandt, Peter; Dengler, Marcus; Krahmann, Gerd; Tanhua, Toste; Visbeck, Martin (2013): Diapycnal oxygen supply to the tropical North Atlantic oxygen minimum zone. Biogeosciences, 10(7), 5079-5093 ... Article in Journal/Newspaper North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Gerd ENVELOPE(-45.750,-45.750,-60.666,-60.666) Tanhua ENVELOPE(27.541,27.541,67.528,67.528)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Climate - Biogeochemistry Interactions in the Tropical Ocean SFB754
spellingShingle Climate - Biogeochemistry Interactions in the Tropical Ocean SFB754
Fischer, Tim
Banyte, Donata
Brandt, Peter
Dengler, Marcus
Krahmann, Gerd
Tanhua, Toste
Visbeck, Martin
Physical Oceanography in the tropical Atlantic oxygen minimum zone ...
topic_facet Climate - Biogeochemistry Interactions in the Tropical Ocean SFB754
description The replenishment of consumed oxygen in the open ocean oxygen minimum zone (OMZ) off northwest Africa is accomplished by oxygen transport across and along density surfaces, i.e. diapycnal and isopycnal oxygen supply. Here the diapycnal oxygen supply is investigated using a large observational set of oxygen profiles and diapycnal mixing data from years 2008 to 2010. Diapycnal mixing is inferred from different sources: (i) a large-scale tracer release experiment, (ii) microstructure profiles, and (iii) shipboard?acoustic current measurements plus density profiles. From these measurements, the average diapycnal diffusivity in the studied depth interval from 150 to 500m is estimated to be 1×10**-5 m2 s**-1, with lower and upper 95% confidence limits of 0.8×10**-5 m2 s**-1 and 1.4×10**-5 m2 s**-1. Diapycnal diffusivity in this depth range is predominantly caused by turbulence, and shows no significant vertical gradient. Diapycnal mixing is found to contribute substantially to the oxygen supply of the OMZ. Within ... : Supplement to: Fischer, Tim; Banyte, Donata; Brandt, Peter; Dengler, Marcus; Krahmann, Gerd; Tanhua, Toste; Visbeck, Martin (2013): Diapycnal oxygen supply to the tropical North Atlantic oxygen minimum zone. Biogeosciences, 10(7), 5079-5093 ...
format Article in Journal/Newspaper
author Fischer, Tim
Banyte, Donata
Brandt, Peter
Dengler, Marcus
Krahmann, Gerd
Tanhua, Toste
Visbeck, Martin
author_facet Fischer, Tim
Banyte, Donata
Brandt, Peter
Dengler, Marcus
Krahmann, Gerd
Tanhua, Toste
Visbeck, Martin
author_sort Fischer, Tim
title Physical Oceanography in the tropical Atlantic oxygen minimum zone ...
title_short Physical Oceanography in the tropical Atlantic oxygen minimum zone ...
title_full Physical Oceanography in the tropical Atlantic oxygen minimum zone ...
title_fullStr Physical Oceanography in the tropical Atlantic oxygen minimum zone ...
title_full_unstemmed Physical Oceanography in the tropical Atlantic oxygen minimum zone ...
title_sort physical oceanography in the tropical atlantic oxygen minimum zone ...
publisher PANGAEA
publishDate 2013
url https://dx.doi.org/10.1594/pangaea.819311
https://doi.pangaea.de/10.1594/PANGAEA.819311
long_lat ENVELOPE(-45.750,-45.750,-60.666,-60.666)
ENVELOPE(27.541,27.541,67.528,67.528)
geographic Gerd
Tanhua
geographic_facet Gerd
Tanhua
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.5194/bg-10-5079-2013
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.81931110.5194/bg-10-5079-2013
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