Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Brandt, Peter; Bange, Hermann W; Banyte, Donata; Dengler, Marcus; Didwischus, Sven-Helge; Fischer, Tim; Greatbatch, Richard J; Hahn, Johannes (2016): On the role of circulation and mixing in the ventilation of oxygen minimum zones with a focus on the eastern tropical North Atlantic. PANGAEA, https://doi.org/10.1594/PANGAEA.860360, Supplement to: Brandt, Peter; Bange, Hermann W; Banyte, Donata; Dengler, Marcus; Didwischus, Sven-Helge; Fischer, Tim; Greatbatch, Richard J; Hahn, Johannes; Kanzow, Torsten; Karstensen, Johannes; Körtzinger, Arne; Krahmann, Gerd; Schmidtko, Sunke; Stramma, Lothar; Tanhua, Toste; Visbeck, Martin (2015): On the role of circulation and mixing in the ventilation of oxygen minimum zones with a focus on the eastern tropical North Atlantic. Biogeosciences, 12(2), 489-512, https://doi.org/10.5194/bg-12-489-2015

Always quote above citation when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Ocean observations carried out in the framework of the Collaborative Research Center 754 (SFB 754) "Climate-Biogeochemistry Interactions in the Tropical Ocean" are used to study (1) the structure of tropical oxygen minimum zones (OMZs), (2) the processes that contribute to the oxygen budget, and (3) long-term changes in the oxygen distribution. The OMZ of the eastern tropical North Atlantic (ETNA), located between the well-ventilated subtropical gyre and the equatorial oxygen maximum, is composed of a deep OMZ at about 400 m depth with its core region centred at about 20° W, 10° N and a shallow OMZ at about 100 m depth with lowest oxygen concentrations in proximity to the coastal upwelling region off Mauritania and Senegal. The oxygen budget of the deep OMZ is given by oxygen consumption mainly balanced by the oxygen supply due to meridional eddy fluxes (about 60%) and vertical mixing (about 20%, locally up to 30%). Advection by zonal jets is crucial for the establishment of the equatorial oxygen maximum. In the latitude range of the deep OMZ, it dominates the oxygen supply in the upper 300 to 400 m and generates the intermediate oxygen maximum between deep and shallow OMZs. Water mass ages from transient tracers indicate substantially older water masses in the core of the deep OMZ (about 120-180 years) compared to regions north and south of it. The deoxygenation of the ETNA OMZ during recent decades suggests a substantial imbalance in the oxygen budget: about 10% of the oxygen consumption during that period was not balanced by ventilation. Long-term oxygen observations show variability on interannual, decadal and multidecadal time scales that can partly be attributed to circulation changes. In comparison to the ETNA OMZ the eastern tropical South Pacific OMZ shows a similar structure including an equatorial oxygen maximum driven by zonal advection, but overall much lower oxygen concentrations approaching zero in extended regions. As the shape of the OMZs is set by ocean circulation, the widespread misrepresentation of the intermediate circulation in ocean circulation models substantially contributes to their oxygen bias, which might have significant impacts on predictions of future oxygen levels.
Related to:
Krahmann, Gerd (2014): Physical oceanography during L'Atalante cruise ATA_IFMGEOMAR-4. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.834325
Krahmann, Gerd (2012): Physical oceanography during L'Atalante cruise ATA03. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.777921
Krahmann, Gerd (2012): Physical oceanography during Maria S. Merian cruise MSM10/1. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.774713
Krahmann, Gerd (2014): Physical oceanography during METEOR cruise M80/1. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.834424
Krahmann, Gerd (2014): Physical oceanography during METEOR cruise M80/2. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.834442
Krahmann, Gerd (2014): Physical oceanography during METEOR cruise M83/1. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.834459
Krahmann, Gerd; Bange, Hermann W (2015): Physical oceanography during POSEIDON cruise POS348. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.848597
Krahmann, Gerd; Bange, Hermann W (2015): Physical oceanography during POSEIDON cruise POS399 in June 2010. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.848614
Stramma, Lothar (2012): Physical oceanography during METEOR cruise M68/2. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.787643
Stramma, Lothar (2012): Physical oceanography during METEOR cruise M68/3. IFM-GEOMAR Leibniz-Institute of Marine Sciences, Kiel University, PANGAEA, https://doi.org/10.1594/PANGAEA.787808
Coverage:
Median Latitude: 5.965065 * Median Longitude: -16.569739 * South-bound Latitude: -5.029000 * West-bound Longitude: -24.333333 * North-bound Latitude: 17.589500 * East-bound Longitude: -0.000167
Date/Time Start: 2011-05-11T21:00:00 * Date/Time End: 2011-07-19T07:07:00
Size:
2 datasets

Download Data

Download ZIP file containing all datasets as tab-delimited text (use the following character encoding: )