Page 2: 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.

New study sheds light on Victoria's future rainfall

New research led by Monash University sheds a new perspective on forecasts of future rainfall in Victoria, showing that recent dry conditions may not fully reflect long-term climate change signals.

Interactive hydrology makes a splash with students

As climate change increases the risk of flooding worldwide, understanding how floods form has never been more important. However, the science behind flooding is notoriously difficult to grasp, involving interactions among ...

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