4.7 Article

Modulation of Bubble-Mediated CO2 Gas Transfer Due To Wave-Current Interactions

Journal

GEOPHYSICAL RESEARCH LETTERS
Volume 49, Issue 22, Pages -

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2022GL100017

Keywords

air-sea interaction; wave-current interactions; gas transfer; wave breaking; submesoscale currents; coupled models

Funding

  1. NSF [OCE 1924686, OCE 2121646, OCE 2122042]

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Wave breaking modulates air-sea fluxes and the interaction between waves and currents affects the bubble-mediated gas transfer coefficients. Submesoscale current gradients can enhance the gas transfer coefficient, especially along temperature fronts and cold filaments. This has the potential to enhance CO2 exchange in regions with increased submesoscale activity.
Wave breaking modulates air-sea fluxes of energy, momentum, heat, and gases. Building on recent advances in the modeling of CO2 gas exchange and wave breaking, we investigate the variability of bubble-mediated gas transfer coefficients due to wave-current interactions. Submesoscale current gradients strongly modulate wave breaking, which can enhance the bubble-mediated gas transfer coefficient along temperature fronts and cold filaments. The enhancement of the gas transfer coefficient is over relatively small areas averaging out over larger regions. However, the correlation between positively anomalous gas transfer coefficients and regions with strong downwelling could potentially enhance CO2 exchange over regions with increased submesoscale activity. An empirical scaling based on the mean wave period, root-mean-square current gradients, and friction velocity can explain the root-mean-square differences of gas transfer coefficients computed from solutions with and without current forcing.

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