Articles | Volume 12, issue 4
https://doi.org/10.5194/os-12-1003-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-12-1003-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Impact of vertical and horizontal advection on nutrient distribution in the southeast Pacific
Bàrbara Barceló-Llull
CORRESPONDING AUTHOR
Universidad de Las Palmas de Gran Canaria, ULPGC, Las Palmas de Gran Canaria, Spain
Evan Mason
Institut Mediterrani d'Estudis Avançats, IMEDEA (CSIC-UIB), Mallorca, Spain
Arthur Capet
CNR, OGS, Trieste, Italy
Ananda Pascual
Institut Mediterrani d'Estudis Avançats, IMEDEA (CSIC-UIB), Mallorca, Spain
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Arthur Capet, Emil V. Stanev, Jean-Marie Beckers, James W. Murray, and Marilaure Grégoire
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We show that the Black Sea oxygen inventory has decreased by 44 % from 1955 to 2015, while oxygen penetration depth decreased from 140 to 90 m. A transient increase of the oxygen inventory during 1985–1995 supported the perception of a stable oxic interface and of a general recovery of the Black Sea after a strong eutrophication phase (1970–1990). Instead, we show that ongoing high oxygen consumption was masked by high ventilation rates, which are now limited by atmospheric warming.
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Short summary
Vertical velocity in the ocean makes an important contribution to the modulation of marine ecosystems through its impact on fluxes of nutrients and phytoplankton. Here, we estimate full 3-D current velocity fields from an observation-based data product. The 3-D currents are used to force a set of particle-tracking (Lagrangian) experiments. The Lagrangian results show that vertical motions induce local increases in nitrate uptake reaching up to 30 %.
Vertical velocity in the ocean makes an important contribution to the modulation of marine...