The document describes different types of rainfall and their formation processes, particularly focusing on convectional, relief, and frontal rainfall in Britain. It highlights the role of mountains and temperature differences in precipitation formation, emphasizing the impact of moisture-laden winds and cooling air. Specific rainfall patterns and conditions are noted, with examples of occurrence across seasons.

1. Types of rainfall Move the items into the correct places on the slide and use custom animation to show the sequence of events Put a correct title on each type of rainfall by removing the other types from the title

2. Mountains on the west coast of Britain forces the air to rise Water vapour Condenses to form clouds Evaporation of water from the ocean Onshore moisture laden winds Air cools down Further cooling leads to precipitation Formation of Convectional / Relief / Frontal Rainfall Occurs in the mountains on the west coast of Britain 1,000 mm 2,000+ mm Under 750 mm

3. Water vapour Condenses to form clouds Air cools down Further cooling leads to heavy precipitation Warm air rises Ground heats up the air Sun’s rays heat up the ground Occurs in Britain in the late afternoon after the maximum heating In the tropical rainforest every afternoon Formation of Convectional / Relief / Frontal Rainfall

4. Water vapour Condenses to form clouds Warm air rises Further cooling leads to precipitation along the Warm Front Air cools down Occurs mainly in winter in Britain but can occur any time of the year Warm moisture laden air from the south meets cold air from the north and forms the Warm Front Formation of Convectional / Relief / Frontal Rainfall Warm air Cold air