If I understand the paper correctly, Southern Hemisphere westerly winds are intensifying due to a natural cycle on the scale of decades. This makes the souther

If I understand the paper correctly, Southern Hemisphere westerly winds are intensifying due to a natural cycle on the scale of decades. This makes the southern ocean warmer (and the arctic colder, but the ocean is mostly in the south). Warm water doesn't take up so much carbon dioxide. (Water takes up carbon to produce carbonic acid, so if the water is warmer it incidentally reduces ocean acidification, a possible benefit?) Or it might be about convection. > The drivers and source of these centennial-scale CO2 jumps are unknown. The proposed mechanisms include enhanced ocean–atmosphere CO2 exchange in the Southern Ocean (via wind-driven upwelling of carbon-rich deep waters or invigorated convection), surface ocean temperature changes (impacting CO2 solubility), biomass burning (via NH subtropical wildfires), or a combination of mechanisms.