Year: 2015
Type: article
Abstract: The role of mesoscale eddies in the uptake of anthropogenic chlorofluorocarbon‐11 (CFC‐11) gas is investigated with a 1/20° eddy‐resolving numerical ocean model of a region of the Southern Ocean. With a relatively fast air‐sea equilibrium time scale (about a month), the air‐sea CFC‐11 flux quickly responds to the changes in the mixed layer CFC‐11 partial pressure ( p CFC‐11). At the mesoscale, significant correlations are observed between p CFC‐11 anomaly, anomalies in sea surface temperature (SST), net heat flux, and mixed layer depth. An eddy‐centric analysis of the simulated CFC‐11 field suggests that anticyclonic warm‐core eddies generate negative p CFC‐11 anomalies and cyclonic cold‐core eddies generate positive anomalies of p CFC‐11. Surface p CFC‐11 is modulated by mixed layer dynamics in addition to CFC‐11 air‐sea fluxes. A negative cross correlation between mixed layer depth and surface p CFC‐11 anomalies is linked to higher CFC‐11 uptake in anticyclones and lower CFC‐11 uptake in cyclones, especially in winter. An almost exact asymmetry in the air‐sea CFC‐11 flux between cyclones and anticyclones is found.
DOI: 10.1002/2014jc010292
Language: English
Subfield: Oceanography
Field: Earth and Planetary Sciences
Domain: Physical Sciences
Open Access status: green
Awards: GEOCHEMICAL ESTIMATES OF NEW PRODUCTION SURPASS THE APPARENT RATE OF NUTRIENT SUPPLY BY VERTICAL MIXING BY A FACTOR OF TWO OR MORE IN SUBTROPICAL OCE, G400575752, Collaborative Research Type 2 - MOBY: Modeling Ocean Variability and Biogeochemical Cycles, Collaborative Research Type 2 - MOBY: Modeling Ocean Variability and Biogeochemical Cycles
OpenAlex ID: W2066720902
