Articles | Volume 18, issue 2
https://doi.org/10.5194/bg-18-755-2021
https://doi.org/10.5194/bg-18-755-2021
Research article
 | 
01 Feb 2021
Research article |  | 01 Feb 2021

Dynamics of the deep chlorophyll maximum in the Black Sea as depicted by BGC-Argo floats

Florian Ricour, Arthur Capet, Fabrizio D'Ortenzio, Bruno Delille, and Marilaure Grégoire

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Cited articles

Anderson, G.: Subsurface chlorophyll maximum in the northeast Pacific Ocean, Limnol. Oceanogr., 14, 386–391, 1969. a
Ardyna, M., Babin, M., Gosselin, M., Devred, E., Bélanger, S., Matsuoka, A., and Tremblay, J.-É.: Parameterization of vertical chlorophyll a in the Arctic Ocean: impact of the subsurface chlorophyll maximum on regional, seasonal, and annual primary production estimates, Biogeosciences, 10, 4383–4404, https://doi.org/10.5194/bg-10-4383-2013, 2013. a
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Argo Data Management Team (Carval Thierry, Keeley Robert, Takatsuki Yasushi, Yoshida Takashi, Loch Stephen, Schmid Claudia, Goldsmith Roger, Wong Annie, McCreadie Rebecca, Thresher Ann, Tran Anh): Argo user's manual V3.4, Ifremer, https://doi.org/10.13155/29825, 2021. a
Beckmann, A. and Hense, I.: Beneath the surface: Characteristics of oceanic ecosystems under weak mixing conditions–a theoretical investigation, Prog. Oceanogr., 75, 771–796, 2007. a, b, c
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This paper addresses the phenology of the deep chlorophyll maximum (DCM) in the Black Sea (BS). We show that the DCM forms in March at a density level set by the winter mixed layer. It maintains this location until June, suggesting an influence of the DCM on light and nutrient profiles rather than mere adaptation to external factors. In summer, the DCM concentrates ~55 % of the chlorophyll in a 10 m layer at ~35 m depth and should be considered a major feature of the BS phytoplankton dynamics.
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