Articles | Volume 19, issue 16
Research article
30 Aug 2022
Research article |  | 30 Aug 2022

Physical mechanisms for biological carbon uptake during the onset of the spring phytoplankton bloom in the northwestern Mediterranean Sea (BOUSSOLE site)

Liliane Merlivat, Michael Hemming, Jacqueline Boutin, David Antoine, Vincenzo Vellucci, Melek Golbol, Gareth A. Lee, and Laurence Beaumont

Data sets

Mediterranean Sea surface CO2 partial pressure and temperature data Liliane Merlivat and Jacqueline Boutin

Deployment of UEA Seaglider sg537 ('Fin') near the Boussole time series site (Mediterranean Sea) with pH/p(CO2) ISFET sensor testing, March - April 2016 J. Kaiser and M. P. Hemming

Short summary
We use in situ high-temporal-resolution measurements of dissolved inorganic carbon and atmospheric parameters at the air–sea interface to analyse phytoplankton bloom initiation identified as the net rate of biological carbon uptake in the Mediterranean Sea. The shift from wind-driven to buoyancy-driven mixing creates conditions for blooms to begin. Active mixing at the air–sea interface leads to the onset of the surface phytoplankton bloom due to the relaxation of wind speed following storms.
Final-revised paper