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Right then Year 9, let's look at a brilliant example of relief rainfall! The Lake District experiences heavy rainfall due to moist air being forced up over the mountains. As the air rises, it cools, condenses and produces rainfall. This is why Scafell Pike and surrounding areas receive over 200 rainy days per year!

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Here's another smashing example of relief rainfall, class! Snowdonia in Wales is one of the wettest regions in the UK, receiving around 3000mm of rain annually. The prevailing westerly winds from the Atlantic Ocean meet the Welsh mountains, creating perfect conditions for relief rainfall.

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Now then students, London frequently experiences frontal rainfall when warm and cold air masses meet. This creates those dreary, grey days with steady rainfall that we're all too familiar with! This type of rainfall is common across the southeast and typically moves from west to east.

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Ah, Manchester! Known for its football and... rain! The city experiences plenty of frontal rainfall due to its location. When warm air from the south meets cold air from the north, we get these fascinating frontal systems. This is why Mancunians always carry a brolly!

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Listen up class! East Anglia gives us brilliant examples of convectional rainfall, especially in summer. The flat farmland heats up quickly, causing air to rise rapidly. This creates those dramatic summer thunderstorms that catch everyone by surprise! Perfect for our weather study.

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Here's something interesting for your notebooks! Cornwall experiences convectional rainfall when warm summer seas heat the air above. This creates those sudden heavy showers that pop up on otherwise lovely beach days. Don't forget your cagoule when visiting the Eden Project!