Chap. 3 Range M. Flashcards
What mountain range causes the rain shadow is Rexburg?
The Sierra-Nevada or Cascade Mountains
Annual Variation in Precipitation
–Variability in precipitation increases rapidly as the annual total drops below 18 inches (450 mm). This greatly increases variability in forage production.
–Forage production is much more erratic from year to year in desert areas than in prairie areas. This increases ranching risk and reduces profitability in desert compared to prairie areas.
Drought
**75% or less of the average annual growing season precipitation
- Intensity and duration determine its severity
-Some plant species may benefit from drought (deep rooted shrubs) due to reduced competition
•Shallow rooted species such as grasses often die
***Factors Determining Precipitation Effectiveness
Intensity and duration—soil texture, slope, plant cover
B. Distribution—season
C. Wind—increases evaporation
D. Temperature—high temperature increases evaporation
E. Relative Humidity—higher the relative humidity, more precipitation
F. Form of precipitation—rain versus snow
Snow
- until it melts
- May extend period of available soil moisture
- Lost from area by:
1. Runoff
2. Evaporationk
3. Sublimation
Plains
- Dry winters, wet summers, moderate total precipitation (10-35 inches annual ppt), grassland.
Pacific
- Wet winters, dry summers, moderate to high total precipitation (15-50 inches annual ppt), cool season herbaceous species.
Southwestern
– Bimodal precipitation (winter and summer), low to moderate total precipitation (5-18 inches annual ppt), cactus and creosote.
Great Basin
- Wet winter and spring, dry summers, low total precipitation (4-16 inches annual ppt), sagebrush and juniper.
Eastern
- Even distribution of precipitation throughout year, high total precipitation (35-55 inches annual ppt), deciduous trees.
Florida
- Summer peak in precipitation but wet all year (50-70 inches annual ppt).
Topography
•refers to the relief (slope) features of a land area.
–Wide differences in topography between the eastern and western United States largely explain differences in climate and vegetation.
–Aspect of slopes has considerable influence on the vegetation and their use by grazing animals.
South-facing slopes support what type of climate?
support grassland and are best used in the spring.
North-facing slopes support what type of climate?
are best used in summer because there is more shade, and forage species are less advanced in growth.
Precipitation
is the most important single factor determining the type and productivity of vegetation in an area.
- forage production increases rapidly as precipitation increases up to 20inches(500mm) per year.
- Above 20 inches of precipitation per year, soil characteristics can assume greater importance than precipitation in determining forage production.
Soil
•Dynamic natural body in which plants grow, composed of mineral and organic materials and living forms.
•The most serious consequence of sustained overgrazing is loss of soil.
–⭐️1000 years is typically required for natural formation of 1 inch of soil. However, 1 inch of soil can be lost within a couple of years of severe overgrazing.
Soil Texture
Size of mineral particles in the soil.
a. Rock b. Gravel c. Sand d. Silt e. Clay
What determines the capacity of soil to hold water?
The water-holding capacity of soil increases as particle size decreases because water clings to surfaces, and small particles have relatively the most surface.
What determines soil texture?
Soil texture designation based on percentages of sand, silt, and clay
Soil Structure
Refers to how soil particles are arranged
–Important because it allows water to enter soil and affects soil capability to store water.
–Soils having a granular structure are most productive for farming and grazing because they optimize water infiltration and storage.
What soil factors affect rangeland productivity?
- Fertility
- Texture
- Structure
- pH
- Depth
- Organic matter
Draw a precipitation pattern in —– area?
Pg 37 top map
What are the categories for soil?
Entisols – Rocky Mountains, youngest soil order
•Aridisols – Southwest desert, often dry
•Gelisols – Tundra soils covered with snow and ice
•Mollisols – Grassland and prairies, high organic matter
•Alfisols – Similar to mollisols but more leached
•Ultisols – Southeast, highly leached
•Oxisols – Hawaii and Puerto Rico, most intensively leached
Desertification
formation of desert like conditions largely through human actions in areas that do not have desert climates. Sahel Region of Africa and China •Uncontrolled livestock grazing •Burning vegetation •Cutting wood •Temporary cultivation •Abandonment of semi-arid to arid lands