Biogeochemical Modelling of upper Ocean Sulfur Dynamics and ITS Impact on Cloud Forming Aerosol

The solar radiation dose in the oceanic upper mixed layer (SRD) has recently been identified as
the main climatic force driving global dimethylsulfide (DMS) dynamics and seasonality. Since
DMS is suggested to exert a cooling effect on the Earth radiative budget through its involvement
in the formation and optical properties of tropospheric clouds over the ocean, a positive relationship
between DMS and the SRD supports the occurrence of a negative feedback between
the oceanic biosphere and climate, as postulated 20 years ago. Such a natural feedback
might partly counteract anthropogenic global warming through a shoaling of the mixed layer
depth (MLD) and a consequent increase of the SRD and DMS concentrations and emission. By
applying two globally-derived DMS diagnostic models to global fields of MLD and chlorophyll
simulated with an Ocean General Circulation Model coupled to a biogeochemistry model
for a 50% increase of atmospheric CO2 and an unperturbed control run, we have estimated
the response of the DMS-producing pelagic ocean to global warming. Our results show a net
global increase in surface DMS concentrations, especially in summer. This increase, however, is
so weak (globally 1.2%) that it can hardly be relevant as compared with the radiative forcing
of the increase of greenhouse gases. This contrasts with the seasonal variability of DMS (1000-
2000% summer-to-winter ratio). We suggest that the ’plankton - DMS - clouds - Earth albedo
feedback’ hypothesis is less strong a long-term thermostatic system than a seasonal mechanism
that contributes to regulate the solar radiation doses reaching the Earth’s biosphere.