Dependent on latitude, the annual range can be between -20°C (-4°F) to 30°C (86°F).
Precipitation
Grasslands receive around 500 to 900 millimeters (20 – 35 inches) of rain per year.
Vegetation
Grasses (prairie clover, salvia, oats, wheat, barley, coneflowers)
Grasslands are generally open and continuous, fairly flat areas of grass. They are often located between temperate forests at high latitudes and deserts at subtropical latitudes. Grasses vary in size from 2.1 m (7 ft) tall with roots extending down into the soil 1.8 m (6 ft), to the short grasses growing to a height of only 20 to 25 cm (8 to 10 in) tall. These short grasses can have roots that extend 1 m (about 3 ft) deep.
The height of grass correlates with the amount of rainfall it receives. Grasslands receive about 500 to 950 mm of rain per year compared to deserts, which receive less than 300 mm and tropical forests, which receive more than 2,000 mm. While temperatures are often extreme in some grasslands, the average temperatures are about -20°C to 30°C. Tropical grasslands have dry and wet seasons that remain warm all the time. Temperate grasslands have cold winters and warm summers with some rain.
The grasses die back to their roots annually and the soil and the sod protect the roots and the new buds from the cold of winter or dry conditions. A few trees may be found in this biome along the streams, but not many due to the lack of rainfall.
Grassland soils develop over centuries. Tropical grassland soils, like tropical forest soils, are highly leached by heavy rainfall and have moderate to poor nutrient humus contents. In temperate grasslands, however, generally light precipitation lets nutrients accumulate in thick, organic upper layers of the soil. Lacking the acidic leaf or pine needle litter of forests, these soils tend to be basic and fertile. Such conditions historically supported the rich growth of grasses on which grassland herbivores fed. They can likewise support rich grazing and crop lands for agricultural communities. Either through crops or domestic herbivores, humans have long relied on grasslands and their fertile, loamy soils for the majority of their food. In short, soils store and deliver the water and nutrients which sustain grassland and shrubland plant and animal populations. Low rates of weathering result in weakly-developed soils that closely resemble the rock from which they were derived. Nutrient turnover in dryland soils is surprisingly rapid, leading to little accumulation of nitrogen, phosphorus, and other plant nutrients.