The ocean's energy spectrum is concentrated at the mesoscale, yet
the impact of mesoscale variability on ocean productivity and biogeochemistry
is not well understood. Studies from the open ocean suggest an enhancing
effect on productivity, but little is known elsewhere. We study here the
impact of mesoscale variability on productivity, biogeochemistry and air-sea
CO2 fluxes using an eddy-resolving model of the California Current System
on the basis of the Regional Ocean Modeling System. We compare our standard
simulation with one that is identical, except that we removed all mesoscale
variations by turning off the non-linear terms in the momentum equations.
This comparison reveals that eddies and other mesoscale variations tend
to suppress biological productivity substantially in this coastal upwelling
system, while their integrated impact on air-sea fluxes of CO2 is relatively
small. We interpret this reducing effect of mesoscale variations as being
driven primarily by a lateral eddy-induced transport that brings warm,
nutrient depleted waters from the offshore closer to shore, thereby suppressing
the effect of Ekman induced upwelling. We suspect a similar impact in other
upwelling areas, whether they are coastal or open ocean.
Presented at ASLO Summer Meeting 2005, Santiago de Compostela/Spain, June 20, 2005 (Session: SS08 - Carbon and Carbonate Fluxes in the Coastal Ocean)