Cloud formation suppressed by biogenic organic emissions

Submicron atmospheric aerosols, although they are not so visible, play a pivotal role in the climate system. They cause temperature variations by scattering or absorbing sunlight, while they also act as cloud condensation nuclei (CCN). Consequently, they can impact cloud cover and the precipitation process. Organic matter, which constitutes up to 90 percent of aerosols, is often attributable to biogenic sources.

Many questions, however, remain as to how differences in variation and quantity of biogenic organics affect aerosols and cloud formation in a cool temperate forest which has vegetation highly susceptible to climate change.

At the Tomakomai Experimental Forest, a cool temperate forest in northern Japan, the researchers of Hokkaido University collected submicron atmospheric aerosols one week at a time for each sample for around two years, resulting in 52 samples. They then analyzed the chemical compositions and CCN activities of the aerosol samples.

Their research revealed a clear seasonal variation of CCN activity, which showed a maximum in summer and a minimum in autumn. Importantly, CCN activity is controlled by the mass ratio of sulfate and water-soluble organics. The ratio of sulfate, which facilitates cloud formation, is higher in summer and that of water-soluble organics is relatively higher in autumn. The study indicates an increased amount of water-soluble organics can coat sulfate particles, suppressing its CCN activity.

Furthermore, the researchers found for the first time that aerosols originating from natural organics emitted from soil and litters (fallen leaves) on the forest floor can suppress cloud formation. This provides a new insight into the conventional belief that tree leaves are the primary source of organic gases and aerosols which can affect the cloud formation.

Assistant Professor Yuzo Miyazaki of Hokkaido University, who led the research, said "In recent years, some studies have pointed out that the amount of organics emitted from the forest floor is similar to, or even larger than, that emitted from tree leaves in cool-temperate or other higher-latitude forested areas. Our research should provide clues to evaluate how differences in the variety and amount of organics in high-latitude zones, which are vulnerable to global warming, will affect cloud formation and the overall climate in the future."