Environmental Factors Affecting Agriculture

Environmental factors affecting agriculture are the natural conditions that decide what can be grown or raised in a place: climate (temperature, rainfall, sunshine and the length of the growing season), relief (altitude, slope and aspect), soil (fertility, texture, depth and drainage) and natural hazards such as drought, flood, frost and pests. In brief: crops grow best within certain temperature and water ranges. Rice needs warm temperatures and plenty of water, wheat grows in cooler, drier conditions, and pasture suits steep, wet or cold land. Technology such as irrigation, fertilizer and greenhouses can reduce these limits, but at a cost.

Understanding the physical limits helps to explain the world pattern of farming and the risks that farmers face. This guide explains the effects of climate, relief, soil and hazards, shows how technology changes the limits, compares crop requirements in a table, works through calculations, outlines the history and corrects common mistakes.

How does climate affect farming?

Temperature controls plant growth. Most crops need a minimum of about 5 °C to grow, and each has an optimum range. Frost can kill tender plants such as bananas or damage blossoms of fruit trees. Growing season is the number of days with suitable temperature, and it decides which crops can ripen: it can be 365 days in the tropics, but only 100 days or fewer in northern regions. Rainfall provides water, and both the amount and the seasonal distribution matter. Too little causes drought, and too much causes waterlogging, disease and flooding. Sunshine influences photosynthesis and the ripening of fruit, such as grapes. Wind can damage crops and erode soil, and hail can destroy a harvest in minutes.

How does relief affect farming?

Altitude lowers the temperature by about 6 to 6.5 °C per 1,000 m and shortens the growing season, so high land is mainly used for grazing. Slope matters because steep land is hard to plow, prone to soil erosion and has thin soil, so machines work best on gentle slopes, and steep slopes may need terracing, as in the rice terraces of the Philippines and the Andes. Aspect is the direction a slope faces. In the northern hemisphere, south-facing slopes receive more sun, are warmer and are preferred for vineyards and orchards, for example along the Rhine and Moselle valleys. Flat, low-lying river plains and deltas offer the best land for large-scale farming but may flood.

How do soils affect farming?

Fertile soils have enough nutrients (nitrogen, phosphorus, potassium), a good amount of organic matter, a balanced texture, good drainage and water retention, and a suitable pH. Deep loam soils are best for many crops. Sandy soils drain too fast and hold few nutrients, heavy clay soils become waterlogged, and thin or stony soils limit root growth. Examples of highly productive soils are the black chernozems of the Ukrainian and Russian steppes, alluvial soils on river floodplains such as the Nile and Ganges, and volcanic soils. Poor soils include the leached soils of tropical rainforests and the thin soils of mountains. Soil acidity matters: for example, potatoes tolerate acid soils better than most crops, and lime can be added to raise the pH.

How do hazards and human factors change the picture?

Natural hazards add risk: drought (as in the Sahel and Australia), floods, hurricanes, frost, locust swarms and plant diseases. Climate change is shifting the zones in which crops grow, increasing heat and drought stress in some regions and lengthening the growing season in others. Human factors can override environmental limits: irrigation allows crops in deserts, greenhouses extend the season and allow tropical plants in cold climates, fertilizers improve poor soils, and plant breeding produces drought-tolerant and short-season varieties. Markets, transport, prices, government support and land ownership also determine what is grown, so the environment sets limits but does not decide alone.

Crop requirements compared

Approximate conditions that suit different crops
Crop Temperature Water Soil and other needs
RiceWarm, about 20–30 °CLarge amounts, often flooded fieldsClay-rich alluvial soil, flat land
WheatCool to warm, dry harvestModerate, about 250–750 mmDeep, fertile loam
MaizeWarm summerModerate to highWell-drained fertile soil
CoffeeMild, no frostHigh rainfall with a dry spellRich, well-drained soil, often on slopes
PotatoesCoolModerateLoose, slightly acid soil
VinesWarm, sunny summersModerate to lowWell-drained slopes

Worked example: season, water and slope

  1. Growing season: a location has 190 days a year with a mean temperature above 5 °C. A wheat variety needs 140 days to mature, so there are 190 − 140 = 50 days to spare. A maize variety that needs 210 days would not ripen.
  2. Temperature at altitude: a farm at sea level has a mean summer temperature of 20 °C. At 1,500 m the temperature falls by 1.5 × 6.5 = 9.75 °C, so it is about 10 °C, too cold for most maize.
  3. Water balance: a field receives 600 mm of rain and a crop needs 750 mm. The deficit is 750 − 600 = 150 mm. One millimeter over 1 hectare (10,000 m2) is 10 m3 of water, so irrigating 150 mm requires 150 × 10 = 1,500 m3 per hectare.
  4. Irrigation for a farm: for 80 hectares, the need is 80 × 1,500 = 120,000 m3 per season.
  5. Slope: a field rises 20 m over a horizontal distance of 100 m. The gradient is 20 ÷ 100 = 20%, which is arctan(0.2) = 11.3 degrees, steep enough to require care against erosion and to limit the use of large machinery.
Temperature falling with altitude compared with the 5 degree growth minimum Altitude above sea level (m) Mean summer temperature (°C) 0 500 1000 1500 2000 2500 0 5 10 15 20 5 °C: minimum for growth about 10 °C at 1,500 m
The worked example: a farm at sea level has a mean summer temperature of 20 °C, and the temperature falls by 6.5 °C per 1,000 m. At 1,500 m it is about 10 °C, too cold for most maize, and at roughly 2,300 m it reaches 5 °C, the minimum most crops need to grow.

How have farmers overcome environmental limits?

Early farmers settled in river valleys and fertile areas, and ancient civilizations such as Mesopotamia and Egypt developed irrigation to use river water. Terracing allowed cultivation on steep slopes in Asia and the Andes. Selective breeding over thousands of years produced crops adapted to different conditions. In the 20th century, synthetic fertilizers, new varieties, mechanization and groundwater pumping extended farming into new areas. At the same time, problems of soil degradation, falling water tables and salinization appeared in some irrigated regions, showing that the limits can be pushed but not removed. Modern research focuses on climate-resilient crops and efficient water use.

Which mistakes are common?

Mistake 1: Looking only at annual rainfall

The timing matters as much as the total. A region with rain only in a short season may not support crops without irrigation.

Mistake 2: Assuming that tropical soils are always fertile

Heavy rain leaches nutrients from many tropical soils, which is why cleared rainforest land often gives poor yields after a few years.

Mistake 3: Thinking that the environment alone decides what is farmed

Technology, markets, prices, culture and policy also shape the choices of farmers.

Mistake 4: Ignoring the effect of aspect and local climate

Two fields in the same region can differ greatly in temperature and frost risk because of slope direction, altitude and shelter.