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Agriculture in Scotland

Farming sector of the economy of Scotland

  • 16 min read
  • 6 chapters

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Through Neolithic, Iron Age and Feudalism

The early modern era saw the impact of the Little Ice Age, which peaked towards the end of the seventeenth century. The closing decade of the seventeenth century saw a slump, followed by four years of failed harvests, in what is known as the "seven ill years", but these shortages would be the last of their kind. After the Union of 1707 there was a conscious attempt to improve agriculture among the gentry and nobility. Introductions included haymaking, the English plough, new crops, crop rotation and encloses were introduced. The resulting Lowland Clearances saw hundreds of thousands of cottars and tenant farmers from central and southern Scotland lose access to land and either become landless agricultural workers or emigrate to the growing industrial cities or elsewhere. The later Highland Clearances involved the eviction of many traditional tenants as lands were enclosed, principally for sheep farming. In the first phase, many Highlanders were relocated as crofters, living on very small rented farms which required other employment to be found.

In the twentieth century Scottish agriculture became more susceptible to world markets. There were dramatic price rises in the First World War, but a slump in the 1920s and 1930s, followed by more rises in World War II. In 1947 annual price reviews were introduced in an attempt to stabilise the market. There was a drive in UK agriculture to greater production until the late 1970s, resulting in intensive farming. There was increasing mechanisation and farming became less labour-intensive. UK membership of the European Economic Community from 1972 began a change in orientation for Scottish farming. Some sectors became viable only with subsidies. A series of reforms to the CAP from the 1990s attempted to control over-production, limit incentives for intensive farming and mitigate environmental damage. A dual farm structure has emerged with agriculture divided between large commercial farms and small pluralised and diversified holdings.

Roughly 79 per cent of Scotland’s total land area is under agricultural production. Cereals accounted for 78 per cent of cropped land area (not total farmed area), while livestock numbers have been falling in recent years. Around 15 per cent of the total land area of Scotland is forested, most in public ownership controlled by the Forestry Commission. Total income from farming has been rising since the turn of the millennium. Aquaculture production is focused on the West and North of the country. Some farm businesses rely on sources of income other than from farming. Scottish agriculture employs around 1.5 per cent of the workforce and contributes to around 1 per cent of the Scottish economy.

Topography and climate

The defining factor in the geography of Scotland is the distinction between the Highlands and Islands in the north and west and the Lowlands in the south and east. The Highlands are further divided into the Northwest Highlands and the Grampian Mountains by the fault line of the Great Glen. The Lowlands are divided into the fertile belt of the Central Lowlands and the higher terrain of the Southern Uplands, which included the Cheviot Hills, over which the border with England runs. The Central Lowland belt averages about 50 miles in width, and contains most of the good quality agricultural land. Scotland is half the size of England and Wales in area, but with its many inlets, islands and inland lochs, it has roughly the same amount of coastline at 4,000 miles. Only a fifth of Scotland is less than 60 metres above sea level.

Scotland's soils are diverse for a relatively small country due to the variation in geology, topography, climate, altitude and land use history. There are very productive arable soils in the east of the country, including some of the most productive for wheat and barley of anywhere in the world. Scotland's soils differ from much of the rest of the UK and Europe and they provide valuable habitats for wildlife and flora. They are largely naturally acidic in nature with high concentrations of organic carbon. They are predominantly coarse textured and often exhibit poor drainage.

The climate of Scotland is temperate and very changeable, but rarely extreme. Scotland is warmed by the North Atlantic Drift and given the northerly location of the country, experiences much milder conditions than areas on similar latitudes. Average temperatures are lower than in the rest of Great Britain. Western coastal areas of Scotland are warmer than the east and inland areas, due to the influence of the Atlantic currents, and the colder surface temperatures of the North Sea. Rainfall totals vary widely across Scotland—the western highlands of Scotland are one of the wettest places in the UK with annual rainfall up to 4,577 mm (180.2 in). In comparison, much of eastern Scotland receives less than 870 mm (34.3 in) annually; lying in the rain shadow of the western uplands. Annual average sunshine totals vary from as little as 711–1140 hours in the Highlands and the north-west up to 1471–1540 hours on the extreme eastern and south-western coasts. Wind prevails from the south-west, bringing warm, wet and unstable air from the Atlantic. The windiest areas of Scotland are in the north and west, with parts of the Outer Hebrides, Orkney and Shetland experiencing over 30 days with gales per year. Vigorous Atlantic depressions, also known as European windstorms, are a common feature of the autumn and winter in Scotland.

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