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Volume 13, issue 4 | Copyright
Ocean Sci., 13, 551-576, 2017
https://doi.org/10.5194/os-13-551-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 06 Jul 2017

Research article | 06 Jul 2017

Decadal oxygen change in the eastern tropical North Atlantic

Johannes Hahn1, Peter Brandt1,2, Sunke Schmidtko1, and Gerd Krahmann1 Johannes Hahn et al.
  • 1GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany
  • 2Christian-Albrechts-Universität zu Kiel, Kiel, Germany

Abstract. Repeat shipboard and multi-year moored observations obtained in the oxygen minimum zone (OMZ) of the eastern tropical North Atlantic (ETNA) were used to study the decadal change in oxygen for the period 2006–2015. Along 23°W between 6 and 14°N, oxygen decreased with a rate of −5.9±3.5µmolkg−1 decade−1 within the depth covering the deep oxycline (200–400m), while below the OMZ core (400–1000m) oxygen increased by 4.0±1.6µmolkg−1 decade−1 on average. The inclusion of these decadal oxygen trends in the recently estimated oxygen budget for the ETNA OMZ suggests a weakened ventilation of the upper 400m, whereas the ventilation strengthened homogeneously below 400m. The changed ventilation resulted in a shoaling of the ETNA OMZ of −0.03±0.02kgm−3 decade−1 in density space, which was only partly compensated by a deepening of isopycnal surfaces, thus pointing to a shoaling of the OMZ in depth space as well (−22±17m decade−1). Based on the improved oxygen budget, possible causes for the changed ventilation are analyzed and discussed. Largely ruling out other ventilation processes, the zonal advective oxygen supply stands out as the most probable budget term responsible for the decadal oxygen changes.

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Recent studies have shown that the eastern tropical North Atlantic is subject to a strong decrease of the oceanic oxygen concentration in the upper 1000 m from the 1960s to today. By analyzing a broad observational data set, this study found an even stronger oxygen decrease in the upper 400 m throughout the past decade, whereas oxygen increase was found below (400–1000 m). Changes in the strength of the zonal currents are the most likely reason for the observed decadal oxygen changes.
Recent studies have shown that the eastern tropical North Atlantic is subject to a strong...
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