Response of the ENSO-driven CO2 flux variability in the equatorial Pacific under high-warming scenario

<div class="page" title="Page 1"> <div class="section"> <div class="layoutArea"> <div class="column"> <p>The El Nin&#771;o&#8211;Southern Oscillation (ENSO) widely modulates the global carbon cycle. More specifically, it alters the net uptake of carbon in the tropical ocean. Over the tropical Pacific, less carbon is released during El Nin&#771;o, while the opposite is the case for La Nin&#771;a. Here, the skill of Earth system models (ESMs) from the latest Coupled Model Intercomparison Project (CMIP6) to simulate the observed tropical Pacific CO₂ flux variability in response to ENSO is assessed. The temporal amplitude and spatial extent of CO2 flux anomalies vary considerably among models, while the surface temperature signals of El Nin&#771;o and La Nin&#771;a phases are generally well represented. Under historical conditions followed by the high-warming Shared Socio-economic Pathway (SSP5-8.5) scenarios, about half the ESMs simulate a reversal in ENSO&#8211;CO₂ flux relationship. This gradual shift, which occurs as early as the first half of the 21st century, is associated with a high CO₂-induced increase in the Revelle factor that leads to stronger sensitivity of partial pressure of CO₂ (pCO₂) to changes in surface temperature between ENSO phases. At the same time, uptake of anthropogenic CO₂ substantially increases upper-ocean dissolved inorganic carbon (DIC) concentrations (reducing its vertical gradient in the thermocline) and weakens the ENSO-modulated surface DIC variability. The response of the ENSO&#8211;CO₂ flux relationship to future climate change is sensitive to the contemporary mean state of the carbonate ion concentration in the tropics. We present an emergent constraint between the simulated contemporary carbonate concentration with the projected cumulated CO₂ fluxes. Models that simulate shifts in the ENSO&#8211;CO₂ flux relationship simulate positive bias in surface carbonate concentrations.</p> </div> </div> </div> </div>