A new publication by researchers from the Department of Earth Sciences at the University of Oxford shows that the relationship between water temperature and the main biological mechanism by which the ocean captures atmospheric carbon dioxide (CO₂) is far more complicated than previously thought.

Drawing on long-term time-series data from oceanographic stations such as the Bermuda Atlantic Time-Series, the research highlights how the quality of currently available data limits our understanding of this critical mechanism in the carbon cycle.

Arctic glaciers are leaking significant amounts of methane, a potent greenhouse gas. Gacial melt rivers and groundwater springs are transporting large volumes of methane from beneath the ice to the atmosphere. This previously unrecognised process could contribute to Arctic climate feedbacks, accelerating global warming.

In a paper published in National Science Review, an international team of scientists found a significant decline of downward surface solar radiation (DSSR) from 1959 to 2014. Greenhouse gases (GHGs) and anthropogenic aerosols contributed equally to the weakening of the DSSR and the role of GHGs was more significant after 1979. Whether DSSR would continue to decrease in the future is highly dependent on emission policies. The implementation of relatively lower aerosols and CO₂ emissions will help to curb the weakening of DSSR and provide a key guarantee for a smooth transition from traditional fossil energy sources to a cleaner one.