- Prevailing winds: The prevailing winds in the UK come from the west or southwest. These winds carry moist air from the Atlantic Ocean, which falls as rain or snow over the western parts of the country. By the time the air reaches the east, it has lost much of its moisture and so there is less rainfall.
- Relief: The east of England is generally lower-lying than the west, and this also affects rainfall patterns. As warm, moist air rises, it cools and condenses, forming clouds and rain. As air descends, it warms and dries, so the lower-lying eastern regions receive less rainfall than the higher western areas.
- Distance from sea: The east of England is further from the sea than the west, and this also contributes to lower rainfall. The sea is a source of moisture, so areas closer to the coast generally receive more rainfall than those inland.
- Human activity: Human activities, such as deforestation and urbanisation, can also affect rainfall patterns. Deforestation reduces the amount of vegetation that can absorb moisture, leading to drier conditions. Urbanisation can create heat islands that reduce cloud formation and precipitation.
As a result of these factors, the eastern parts of England are generally drier than the western parts, with an average annual rainfall of around 600mm in the east compared to around 1,200mm in the west.