Year: 2020
Type: article
Abstract: . Ocean color observations show semiannual variations of chlorophyll in the Atlantic cold tongue with a main bloom in boreal summer and a secondary bloom in December. In this study, ocean color and in situ measurements, and a coupled physical-biogeochemical model are used to investigate the processes that drive this variability. Results show that the main phytoplankton bloom in July-August is driven by a strong vertical supply of nitrate in May-July and the secondary bloom in December is driven by a shorter and moderate supply in November. The upper ocean nitrate balance is analyzed and shows that vertical advection controls the nitrate input in the equatorial euphotic layer and that vertical diffusion and meridional advection are key in extending and shaping the bloom off equator. Horizontal advection mostly acts to bring nitrate low water below the mixed layer. Our results also give insights on the influence of intraseasonal processes in these exchanges. Observations and model show that the Equatorial Undercurrent brings low-nitrate water (relatively to off-equatorial surrounding waters) but still rich enough to enhance the cold tongue productivity.
Source: Biogeosciences
Institutions: Université Toulouse III - Paul Sabatier, Laboratoire d’Études en Géophysique et Océanographie Spatiales, Observatoire Midi-Pyrénées, Institut de Recherche pour le Développement, Institut de Recherche pour le Développement, University of Cape Town, Centre National de la Recherche Scientifique, Sorbonne Université, Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques, Structure et Instabilité des Génomes
Language: English
Subfield: Oceanography
Field: Earth and Planetary Sciences
Domain: Physical Sciences
SDG: Life below water
Open Access status: gold
Estimated APC paid: $1,628
Award: G6368918290
OpenAlex ID: W2973987475
