Follow a water molecule from vapor to rain, snow, ice, or hail.
Precipitation begins when cloud droplets or ice crystals grow large enough to fall. Temperature and humidity through the atmosphere determine whether they remain snow, melt into rain, refreeze into sleet, or freeze on contact at the surface.




Rain forms from liquid droplets or melted ice particles.
Learn MoreSnowflakes grow as ice crystals in cold clouds.
Learn MoreSleet is made of ice pellets.
Learn MoreFreezing rain is liquid when it falls but freezes on cold surfaces.
Learn MoreHail grows inside strong thunderstorm updrafts.
Learn MoreSnow crystals often show sixfold symmetry.
Learn MoreRain gauges measure liquid precipitation.
Learn MorePrecipitation is part of the global water cycle.
Learn MoreWarm clouds can grow raindrops through collision and coalescence, while many midlatitude storms begin with ice crystals aloft.
Temperature and humidity influence crystal shapes.
Snow melts in a warm layer, then refreezes before reaching the surface.
It can coat roads, trees, and power lines with dangerous ice.
Ice stones can make repeated trips through supercooled water before becoming too heavy for the updraft.
The molecular structure of ice gives snowflakes their hexagonal pattern.
Snow is measured by depth and by how much liquid water it contains when melted.
Water evaporates, condenses, falls, infiltrates soil, flows through rivers, freezes, melts, and returns to the ocean and atmosphere.