Deep winter convection and phytoplankton dynamics in the NW Mediterranean Sea under present climate and future (horizon 2030) scenarios.

As shown by the highly significant correlation in Fig. 7d , the decrease in SST drives the increase in surface density, which reduces vertical stratification.

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SeaWiFS, on the contrary, shows a positive trend in the surface Chla concentration, though SeaWiFS has no data available from 2011 onwards in the NASA webpage.

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Two of the three Chla series (MODIS and model) show a decreasing trend in bloom intensity, which is matched by a decreasing trend on the extension of the DC area.

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