What weather is associated with warm and cold fronts?
A warm mass of air will generally hold moisture picked up as it passes over large areas of water though the process of evaporation. As this warm moist air rises it cools and the water vapour condenses into rain – this is known as the dewpoint. So a warm air mass tends to bring with it plenty of rain and drizzle. As a warm front extends further forward the higher up you go, this rain frequently starts to fall before the front reaches you at ground level. Once the front passes over, the rain often eases off but occasional drizzly patches are likely to follow on behind in the warm sector. A cold air mass has a much smaller moisture capacity so there isn’t the same extensive rain as in a warm air mass. However, as a cold front comes in and drives under the warm front, the warmer and moist air will be forced upwards. As the warm air is pushed higher, the moisture it carries condenses and falls as rain. This is why a lot of heavy rain is produced along a cold front but once the cold air mass
