Terrestrial Biomes Notes
Terrestrial Biomes
Terrestrial biomes are categorized by their vegetation, rainfall, and climate.
Essential Knowledge:
Major terrestrial biomes: taiga, temperate rainforests, temperate seasonal forests,
Biome Characteristics
Biome Definition: An area that shares a combination of average yearly temperature and precipitation (climate).
The organisms in a biome are uniquely adapted to live there.
Example: Camels and cacti in deserts have water-preserving traits.
Example: Shrubs and wildflowers in grasslands store energy in roots to recover from fire.
Latitude (distance from the equator) determines temperature and precipitation, leading to predictable biome patterns.
Temperature and Precipitation
Temperature: Warmest at the equator, coldest at the poles due to the angle at which the sun hits the Earth.
Precipitation: Global rainfall depends on global wind circulation, driven by the sun.
Solar energy heats air at the equator, causing it to rise. The rising air cools, and moisture falls as rain.
Drier air spreads north and south and sinks at around 30 degrees latitude.
Temperature & Precipitation Relationship to Biomes
Low Temperature, Low Rainfall: Tundra
Low Temperature, High Rainfall: Coniferous Forest (Taiga)
Warm Temperature, Low Rainfall: Desert
Cool Temperature, Low Rainfall: Temperate Grassland
Cool Temperature, High Rainfall: Temperate Deciduous Forest, Temperate Rainforest
Warm Temperature, High Rainfall: Savanna, Tropical Deciduous Forest, Tropical Rainforest
Tropical Rainforest
Highest precipitation.
Most stable temperature due to high humidity.
Large tropical trees.
Limiting factor for plants: sunlight; epiphytes are common.
Highest biodiversity of terrestrial biomes.
Nutrient-poor soils because decaying organic matter is quickly absorbed by vegetation.
Desert
Hot with extremely low rainfall.
Located around 30° north and south of the equator.
Plants and animals have adaptations for low precipitation.
Savannah/Tropical Grassland
Open grassland with scarce shrubs and trees.
Located between rainforests and deserts.
Warm temperatures year-round (tropical).
Periodic fires occur.
Has wet and dry seasons.
Not enough precipitation to become forests, but enough not to be a desert.
Temperate Grasslands
Cooler temperatures than tropical grasslands.
Less dramatic wet and dry seasons.
Enough rain to sustain grasses (prairies), but not enough to grow forest.
Much lower biodiversity than tropical grasslands.
Known for having the richest soils.
Examples: Great Plains of America, Russian steppes.
Where the corn belt is.
Temperate Rainforest
Receive a lot of year-round rainfall.
Large old-growth trees.
Higher latitudes than tropical rainforests, so temperatures are cooler.
Alaska has the most old-growth forests in the US.
Temperate Deciduous Forest
Mid-latitude forest.
Dominated by deciduous trees (oak, hickory, elm, maple, ash) that lose leaves in winter.
Moderate rainfall.
Experience all four seasons.
Coniferous Forest, Taiga, Boreal
Largest terrestrial biome.
Higher latitude than deciduous forests.
Coniferous trees are pine trees that don’t lose leaves in winter.
Shorter growing season than deciduous forests (colder, less rain).
Example: Redwood forest.
Chaparral
Coastal biome.
Hot, dry summers and mild, rainy winters.
Spiny evergreen shrubs.
Maintained by fire (dry summer); needed for some seeds to germinate.
Tundra
A cold desert (very little precipitation).
Bitter cold, high winds.
Very short growing season.
Permanent ice (permafrost) underlies the surface.
Restricts plants from having deep roots; therefore, no trees.
Found in the Arctic (far north) and high mountains.
Human Impacts: Deforestation
Tropical Rainforest:
Amazon: agricultural land for crops (mostly soy) and cattle.
Indonesia: agricultural land for palm oil.
Results in loss of biodiversity and release of CO_2.
US:
Timber operations
More regulated (government rules, regulations, oversight; penalties for infractions, selective-cutting).
Human Impacts: Soil Erosion
Modern agricultural practices are degrading soil.
Tilling/ploughing before planting
Compaction & overgrazing by livestock
SalinatioHeating of the planet is causing weather patterns and biomes to shift, altering biodiversity.n: over-irrigation leads to a build up of salts.
US farmers have to add more and more fertilizer to get the same yield.
Human Impacts: Climate Change
Plants: Extended growing seasons.
Animals: Changing migration patterns.
Solutions: switch to renewables, tax breaks or rebates for the use of renewables, impose a “carbon tax” for use of fossil fuels.