ENSO-driven variability of denitrification and suboxia in the Eastern Tropical Pacific Ocean

In the mean, these two ODZs are responsible for about 15 to 40% of all fixed N loss in the ocean, but little is known about how this loss varies in time. Here we use a hindcast simulation with the ocean component of the National Center for Atmospheric Research (NCAR) Community Earth System Model over the period 1948 to 2009 to show that the El Nino-Southern Oscillation (ENSO) drives large variations in the rates of WCD in this region.

During mature La Nina (El Nino) conditions, peak denitrification rates are up to 70% higher (lower) than the mean rates. This large variability is the result of wind-driven changes in circulation and isopycnal structure concurrently modifying the thermocline distribution of O-2 and organic matter export in such a way that the response of WCD is strongly amplified. During average La Nina (El Nino) conditions, the overall changes in ODZ structure and primarily the shoaling (deepening) of the upper boundary of both ODZs by 40 to 100 m explains 50% of the changes in WCD in the North Pacific and 94% in the South Pacific.