Many of the concepts on this website are applicable to ecosystems where grasses and sedges are relatively abundant. Examples of how environmental characteristics affect drought risk and recovery are focused on environmental variations in the Great Plains.
The Great Plains
The Great Plains is a historically grass-dominated landscape occurs in three Canadian provinces and ten US states.
The semi-arid zone (depicted in yellow at right) is generally characterized by annual precipitation of 10 to 20 inches (30-year average). In semi-arid regions, drought can be severe enough to impact herbage production for multiple years. The combination of grazing stress and drought stress results in declines in ecological condition in this region.
A transition zone occurs between the semiarid and sub-humid climate zones to the east.
The sub-humid climate zone is characterized by relatively high humidity and cloud cover which diminishes the rate at which summer evening temperatures decline compared to the semiarid zone. In this zone (where average annual precipitation is more than 28 to 30 inches), drought effects on plant communities are often short lived. However, season-long continuous grazing during the growing season will still result in serious declines in range condition.