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Biosphere
Sum total of places in which organisms live
Encompasses the entire earth
The distribution of organisms (biogeography)
is affected by:
Geologic history
Topography
Climate
Other species
Biomes
a region of land characterized by habitat conditions and community structure
Climate
the average weather condition of a region
Latitudinal Impacts on Sunlight
High latitudes cause a particular ray of sunlight to pass through more atmosphere and is distributed over a wider land area than other rays of sunlight at lower latitudes
Tropical regions receive two and a half times as much solar radiation as polar regions
Climate Factors
Solar radiation
Seasonality
Air flow
Precipitation
Ocean currents
Higher Latitude
experiences more extreme seasonal variations
Opposite Hemispheres
experience opposite seasonal variations
Summer Solstice
Northern hemisphere is most tilted toward sun; has it’s longest day
Autumn Equinox
Sun’s direct rays fall on equator; length of day equals length of night
Winter Solstice
Northern Hemisphere is most tilted away from sun; has it’s shortest day
Spring Equinox
Sun’s direct rays fall on equator fall on equator; length of day equals length of night
Global Air Circulation Patterns (Northern Hemisphere)
At 0 degrees, Warm, moist air cools as it rises, causing rainfall
Around 30 degrees latitude, some of the cool, dry air sinks, and is then deflected both North and South
As air travels north, it warms and rises. The clash of moist, warm air and cold polar fronts produces rain at about 60 degrees latitude
Cool, dry air sinks near the poles
Patterns are inverted in the Southern Hemisphere
Precipitation
Solar radiation and air circulation are responsible for global patterns of precipitation
The Coriolis Effect
An object travelling in the straight line across a rotating path appears to travel in an arc
Consider points A and B on a rotating record
Both travel around and arrive at the green line at the same time (same period)
However, B travels a greater distance and must therefore be moving faster than A
Movement of Air
Earth’s rotation causes winds to curve east or west
air circulation established by six giant convection cells
Ocean Currents
Patterns in air circulation drive surface currents
Coastal Wind Patterns
Oceans mitigate temperatures
Breeze blows in direction of warmer region
direction varies with time of day
Rain Shadows
Air rises on the windward side, loses moisture before passing over the mountain
Tundra
Northernmost biome; plants grow in shallow topsoil over a layer of permafrost
Brief growing season; winter winds cause tundra plants to be very short
Boreal Forests
Also called the Taiga
Consists mainly of coniferous forests
Temperate Deciduous
Grow at middle latitudes with abundant rainfall
Trees lose their leaves in the winter
Grasslands
Grows where winters are cold, summers are warm, and rainfall is moderate
Chaparral
Coastal biome dominated by dense, woody shrubs and trees that resprout after periodic fires
Occurs where winters are mild and wet and summers hot and dry
Desserts
Arid regions low precipitation
Tropical Forests
High temperatures and precipitation • Species-rich
Nutrient-poor soil
Aquatic Biomes
Freshwater –
Streams, rivers
Lakes
Ocean
Estuaries
Coastal
Open Ocean
Lakes
Bodies of standing water that accumulate in basins
Fed by rainfall and streams and rivers that drain surrounding watersheds
Oligotrophic
Low in nutrients, high in oxygen
Eutrophic
Rich in nutrients and organic matter
Oceans
Estuaries
Intertidal zones
open ocean