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.

How silver iodide triggers ice formation at the atomic level

No one can control the weather, but certain clouds can be deliberately triggered to release rain or snow. The process, known as cloud seeding, typically involves dispersing small silver iodide particles from aircraft into ...

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