Source: Journal of Geophysical Research: Oceans
At less than 1 millimeter thick, the ocean skin—the ocean’s uppermost layer—plays an outsized role in marine processes, orchestrating heat and chemical exchange between the sea and sky via diffusion. The water of the skin is cooler by about 0.2–0.3 K and has higher salinity than the water at even just 2 millimeters depth.
Since it was first described in 1967, scientists have grappled with the skin’s influence on carbon uptake and the global ocean carbon sink. Understanding its role is critical: Between 2011 and 2020, the ocean absorbed 26% of all human-generated carbon dioxide emissions, and variables that affect ocean carbon sequestration contribute to governing the carbon cycle and climate change.
Bellenger et al. toggled oceanic temperature and salinity gradients to represent the ocean skin over 15 years (2000–2014) in an Earth system model, assessing how these changes altered the amount of carbon absorbed by the ocean. The work represents the first model-based estimate of the ocean skin’s influence on ocean-atmosphere carbon dioxide exchange.
Including the representation of the skin in the Earth system model led to a 15% increase in the simulated ocean carbon sink, the researchers found—a figure consistent with past estimates. However, when they allowed the ocean skin to respond to changing ocean carbon concentrations in the model, the effect on the sink was substantially reduced. With the dynamic skin, its contribution to the simulated ocean carbon sink was closer to 5%.
The research shows the importance of including the ocean skin in future climate and carbon modeling efforts, the authors say. And it demonstrates that an interactive parameterization of the ocean skin yields a more accurate model that reduces regional errors in carbon dioxide flux. (Journal of Geophysical Research: Oceans, https://doi.org/10.1029/2022JC019479, 2023)
—Aaron Sidder, Science Writer