Seasonal variability and drivers of air-sea CO2 exchange in the Arabian Sea
In order to diagnose the physical, chemical, and biological processes creating these discrepancies, we use a high-resolution (5-km) hydrodynamic model, the Regional Oceanic Modeling System (ROMS), coupled to a nitrogen-based nitrogen-phytoplankton-zooplankton-detritus (NPZD) ecosystem model with an implemented carbon chemistry module initialized and forced with climatological fields. With increased horizontal resolution, maximum CO2 outgassing correctly occurs during the summer Monsoon, and the annual CO2 flux is increased. Additionally, we elucidate the dominant roles of dissolved inorganic carbon (DIC) and temperature in determining CO2 flux in the Omani upwelling region and offshore, respectively. Sensitivity experiments also highlight the relative role of circulation and biogeochemical processes in contributing to these factors.
Establishing a seasonal baseline of the drivers responsible for parameters such as pCO2 and pH in the AS is necessary in its own right due to their impact upon marine ecosystems, but it is furthermore essential for projecting how future climate change impacts will modify the role of the AS as a source of CO2 to the atmosphere.
Reference: Sarma et al., 2013 doi: 10.5194/bg-10-7035-2013