Penn geophysicists Hugo Ulloa and Douglas Jerolmack and colleagues have uncovered Earth-sculpting processes that result from the formation of snowball-like aggregates they call “sandballs” that take on two shapes: peanut-shaped structures with liquid cores and stable, donut-shapes—with airy centers—that behave like rigid solids. Their findings provide fundamental insights into erosion and will broaden scientific understandings of landscape change, soil loss, and agriculture.

Researchers typically analyze images taken by geostationary satellites to identify regions of the sky where contrails form, but new research shows adding images taken by low-Earth-orbiting satellites would help identify many more such regions. Pilots could avoid these regions to reduce aviation’s climate impact. 

Satellite and reanalysis data show aerosol changes in the Northern and Southern Hemispheres largely cancel out, shifting attention to cloud changes due to surface warming and natural climate variability.

The climate is changing and nowhere is it changing faster than at Earth’s poles. Researchers at Penn State have painted a comprehensive picture of the chemical processes taking place in the Arctic and found that there are multiple, separate interactions impacting the atmosphere.