Biomes and the Biosphere Flashcards
Atmospheric envelope
- clean, dry air at Earth’s surface
- 70% N
- 21% O
- 1% Ar
- 0.003% CO2
- 0.00005% ozone
Greenhouse effect
- heat trapped in earth’s atmosphere by greenhouse gasses
- water, CO2, methane, ozone, nitrous oxide, chlorofluorocarbons (CFCs)
- absorb infrared and reemit it back to earth
- 30% reflected by clouds + particles
- 70% absorbed by atmosphere or surface
ozone
- filters harmful UV radiation
- absorbs UV, but breaks its bonds in the process
- CFCs break the bonds too and reduce ozone layer
Tilt of Earth’s axis
- uneven heating
- seasons
- drives air circulation and precipitation patterns
- tropics get most direct sunlight (area per unit light) –> 23.5 N to 23.5 S
Air Circulation
- warm, moist air rises, cools, condenses, and rains
- cool, dry air falls back to surface
- Polar cells –> towards the earth and towards the pole
- Ferrel cells –> opposite from closest polar
- Hadley cells–> opposite from closest Ferrel
Coriolis effect
- apparent deflection of the winds
- move clockwise in northern hemisphere
- move counterclockwise in southern hemisphere
- wind is fastest at equator
Ocean circulation
- follows prevailing winds
- currents carry cool water to equator from poles and warm water from the equator to the poles
- air is cooled or warmed by these currents before passing over land
Gulf stream
- made from central american land bridge
- affects climates as far away as the British isles
3 main factors that contribute to storms
- water temperature (temperature)
- wind shear (wind)
- atmospheric moisture (rain)
Mointain’s + water effect on climate
- in U.S. wind blows from west
- wind causes air to rise, cool, and condense on west side of mountain
- cool, dry air descends on east side of mountain (rain shadow)
Mountain shadow deserts
- east side of mountains in temperate zones
- west side of mountains in tropical zones
El Nino
off coast of Peru
- usually wind goes westward and warms over western pacific while picking up moisture
- during El nino, the eastern pacific is unusually warm –> causes storms in the east and droughts in the west
El nino affect on Great Salt Lake
- more storms raise levels 3.7 m
- salinity drops by 50 g/L
- lake invaded by predatory insect
- brine shrimp went from 12000 - 74 per m^3
- a bunch of phytoplankton
- eventually went back to normal
Bodies of water
- large bodies of water govern climate of nearby land
- Day: warm air rises over land, cool breeze from water
- Night: warm air rises from water and moves out from land
Photic zone
- epipelagic region of ocean that’s reached by light
- inhabited by phytoplankton and zooplankton
- produce 1/4 of oxygen for biosphere
Thermocline
separates warm water from cold water
-winter and summer (?)
Turnover
mixing of oxygenated surface water with deeper, nutrient-rich water
- semi annual
- fall and spring
Types of coral reefs
- fringing reefs = hug the shore of continents
- barrier reefs = stand between ocean and lagoon
- coral atolls = coral inlets built up from submerged ocean islands
Shallow marine water
- reefs and kelp beds when there’s sunlight –> limited by temp –> very productive and diverse
- cleaned and feuled by currents
estuaries
- productive, nutrient rich transition bt ocean and river
- water levels very spatially and temporally due to tides
- nutrients driven by ocean tides and river flow
Saltmarshes and mangroves
- concentrated along low lying coasts
- saltmarsh grasses and algae are major producers and attract a bunch of animals
- carbon sequestration
climography plots
- leslie holdrige
- temp on y axis
- rain on x axis
climate diagram
- temp on right
- rain on left
- months on x axis
How do we catagorize terrestrial biomes?
- plants
- climate (temp and rain)
also distribution and animals
serotiny
Jack pine is seratinous bc its cones only open to expose seeds when its super hot bc of a forest fire
Convergent evolution in dif biomes
- similar characteristics due to similar environments
- cacti in north america and euphorbs in african desert
- dif evolutionary lineages
Tropical wet forests
- vertically layered
- competition for light –> broad leaves + lateral growth
- highest diversity of terrestrial biomes
- high productivity
- low soil nutrients
- water is NOT limiting –> plants shed water
- stratification/specialization
- understory + canopy leaves are evergreen
- thin, smooth bark
- buttress roots
Tropical dry forests
- deciduous leaves
- thick corky bark with thorns and spikes
- small leaves
- flower during dry season
Tropical Savana
- tropical grassland
- 10-20 N and S
- dry season is 8-9 months
- temp varies seasonally (usually 24-29)
- grasses, sedges, and herbs with occasional tree
- vegitation is resistant to drought
- trees are deciduous and less than 20 m tall
Deserts
- 30 N and S
- less than 30 cm rain per year
- temp varies seasonally
- plants resistant to heat + desication –> small leaves and good water storage
- animals can conserve water and some are nocturnal
Mediterranean Woodland, Shrubland and
Chapparal
- “chapparal” in US
- fires 600-700 degrees
- soil is hydrophobic –> has waxy resin from burnt plants that forms impermeable underground layer
- torrential rains
- firestorms help some with serotinous cones
Temperate Grassland
- rain and temp is highly seasonal
- most rainfall in spring
- summers are hot and dry
- plants are adapted to drought and fire
- Disturbance is important for community continuity
Temperate Deciduous Forests
- rains year round
- winters = 0 temp, summers = 35
- animals hibernate or migrate to avoid winter
- dominant plants deciduous in Northern hemisphere; evergreen in Australia
Boreal Forest or Taiga
- biggest biome
- North East North America and Eurasia
- rain varies — some have droughts, but coasts are wet
- cold winters, hot summers
- slow decomposition –> reduces nutrient cycling
- store tons of carbon –> boreal forests have 20% more than tropical and temperate forests combined
- Taiga has 30% of all terrestrial carbon
Tundra
- arctic tundra and alpine tundra
- winters below 30, summers around 10
- permafrost (frozen layer of soil) prevents plant root growth
- rains 20-60 cm in arctic and 100 cm in alpine
- home to mosses, lichen grasses, forbs, dwarf trees/shrubs, musk ox, carribeau, reindeer, bears, wolves, foxes, and birds