Aerosol–cloud interactions
Airborne particles change how clouds form and reflect sunlight. How much cooling do those changes produce, across different clouds and weather conditions?
Past climate shifts, cloud feedbacks, atmospheric mixing and the future of ice sheets.
Subjects: Climate and atmosphere
Airborne particles change how clouds form and reflect sunlight. How much cooling do those changes produce, across different clouds and weather conditions?
How will low clouds change under sustained warming, and how will that change affect Earth’s energy balance?
Air contains interacting eddies over an enormous range of sizes. How can their combined effect on heat, momentum, and pollutants be predicted reliably?
A tall Antarctic ice cliff could break up faster than ice flows forward. Whether this can sustain accelerating retreat depends on competing deformation and failure processes.
Why did the dominant rhythm of ice ages change about a million years ago?
What drove Greenland’s repeated rapid warmings during the last ice age?
Which carbon sources triggered and amplified the rapid warming about 56 million years ago?