A transition, not a wall

On a map, a front is just a line. In the atmosphere, it is a three-dimensional, usually sloping transition zone. The line marks its approximate position at the surface. Rain may start well ahead or become heavier behind it.

The main types of front

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Front

What happens?

What often follows

Warm front

Warmer air advances and rises over colder air.

Increasing layered cloud and prolonged precipitation.

Cold front

Colder air advances and lifts warmer air.

A wind shift, cooling, showers or thunderstorms.

Occlusion

A cold front catches a warm front and lifts warm air away from the surface.

Often widespread cloud and precipitation.

Stationary front

The boundary moves very little.

Persistent conditions, sometimes with prolonged rain.

Typical does not mean guaranteed

Not every cold front produces a thunderstorm, and not every warm front brings steady rain. Moisture, stability and the strength of lifting all matter. Sometimes a front is most noticeable as a change in wind direction.

When will it arrive?

Front charts show the broader picture. Current observations, radar and short-range forecasts are better for local timing. A line on the map is not an appointment scheduled to the minute.

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