Scotland

Climate

The climate of Scotland is temperate and oceanic, and tends to be very changeable. As it is warmed by the Gulf Stream from theAtlantic, it has much milder winters (but cooler, wetter summers) than areas on similar latitudes, such as Labrador, southern Scandinavia, the Moscow region in Russia, and the Kamchatka Peninsula on the opposite side of Eurasia. However, temperatures are generally lower than in the rest of the UK, with the coldest ever UK temperature of −27.2 °C (−17.0 °F) recorded at Braemar in the Grampian Mountains, on 11 February 1895. Winter maxima average 6 °C (42.8 °F) in the Lowlands, with summer maxima averaging 18 °C (64.4 °F). The highest temperature recorded was 32.9 °C (91.2 °F) at Greycrook , Scottish Borders on 9 August 2003.

The west of Scotland is usually warmer than the east, owing to the influence of Atlantic ocean currents and the colder surface temperatures of the North Sea. Tiree, in the Inner Hebrides, is one of the sunniest places in the country: it had more than 300 hours of sunshine in May 1975. Rainfall varies widely across Scotland. The western highlands of Scotland are the wettest, with annual rainfall in a few places exceeding 3,000 mm (118.1 in). In comparison, much of lowland Scotland receives less than 800 mm (31.5 in) annually. Heavy snowfall is not common in the lowlands, but becomes more common with altitude. Braemar has an average of 59 snow days per year, while many coastal areas average fewer than 10 days of lying snow per year.