Geographical Factors
* Prevailing Winds: The prevailing winds in the North Atlantic Ocean carry moist air from the south-west towards the British Isles. As this air rises over the high ground of the Highlands of Scotland, it cools and condenses, leading to frequent rainfall.
* Orographic Lift: The mountainous terrain of the Highlands acts as a barrier to the prevailing winds, forcing them to rise and cool rapidly, resulting in heavy rainfall on the windward side (the western slopes) and a rain shadow effect on the leeward side (the eastern slopes).
* Long Coastline: The North West of Scotland has a long and deeply indented coastline, with numerous fjords and sea lochs. This increases the surface area over which moisture-laden air can rise and condense, leading to higher rainfall.
Meteorological Factors
* Low Pressure Systems: The North Atlantic is a frequent breeding ground for low-pressure systems, which bring wet and windy weather to the British Isles. These systems often track northeastward across the Atlantic, bringing persistent rainfall to the North West of Scotland.
* Frontal Systems: When warm, moist air from the Atlantic meets colder air over the North West of Scotland, it creates a frontal boundary, where the air masses collide and generate rainfall. These frontal systems can remain stationary or move slowly, leading to prolonged rainfall.
The combination of these geographical and meteorological factors makes the North West of Scotland the wettest part of the British Isles, with average annual rainfall exceeding 4,000 mm (160 inches) in some areas.