Page 3: Research news on precipitation (atmospheric)

Atmospheric precipitation refers to all forms of water, liquid or solid, that condense from atmospheric water vapor and fall to the Earth’s surface under gravity, including rain, snow, sleet, freezing rain, and hail. It is governed by microphysical processes such as nucleation, droplet and ice-crystal growth, collision–coalescence, riming, and aggregation within clouds, and by dynamical processes like uplift, frontal systems, and convective motions. Precipitation is quantified using intensity, duration, phase, and spatial distribution, and is central to the hydrological cycle, energy budget, and climate system, serving as a key output variable in weather prediction and climate models.

Why rainfall remains hard to predict in a warming world

A new study led by the University of Oxford and ETH Zurich reveals that a key part of the climate system—the large-scale wind patterns that determine where rain falls—can be underestimated by current climate models, helping ...

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