#Aerosols and #Clouds in polluted regions grow faster. This video by our researcher Shravan Deshmukh describes how regional #aerosol #hygroscopicity influences #radiative #forcing globally > https://www.youtube.com/watch?v=ifx-M9-SrBA - From Behind the Paper @springernature https://communities.springernature.com/posts/regional-aerosol-hygroscopicity-influences-radiative-forcing-globally on 10.1038/s43247-026-03505-z https://www.nature.com/articles/s43247-026-03505-z in
@commsearth @nature.portfolio
Regional to Global impact and how aerosols and clouds in atmosphere influences climate.

YouTube

#EarthSystem: "Our results highlight the importance of region-specific #aerosol parameterizations as a crucial step towards reducing uncertainties in the estimation of direct radiative forcing in next-generation #climate models."

https://phys.org/news/2026-05-urban-aerosols-faster-polluted-air.html?utm_source=nwletter&utm_medium=email&utm_campaign=daily-nwletter

Urban aerosols grow faster in polluted air, sharpening climate model gaps

Aerosols and clouds play a key role in Earth's climate budget. However, the extent to which they reflect solar energy depends heavily on how much water the particles can absorb. This so-called hygroscopicity has so far been represented in a simplified manner in climate models. An international research team led by the Leibniz Institute for Tropospheric Research (TROPOS) has now demonstrated through a global study that the models are not precise enough, particularly in urban regions.

Phys.org

Wildfire dark brown carbon has strong global warming effects

Conventional understanding has held that brown #carbon—a type of organic #aerosol from #biomass burning—mainly absorbs sunlight in the near-ultraviolet range, giving it only a limited #climate impact. However, growing observations show that some #wildfire-derived #BrownCarbon appears dark brown or nearly black, absorbing light well into the visible spectrum. This "dark brown carbon" has been largely missing from global climate assessments.

The results show that wildfire-derived brown carbon has a global direct radiative effect of +0.097 W/m², with an uncertainty range of +0.050 to +0.276 W/m². Notably, the upper bound of this estimate (0.276 W/m²) exceeds the radiative contribution of black carbon (0.163 W/m²).

https://phys.org/news/2026-05-wildfire-dark-brown-carbon-strong.html

#ClimateScience