C6 Change of Ecosystems Flashcards
LAYERS OF THE ATMOSPHERE: troposphere
- order
- features
1st layer
- approx 10-15km high
- gets colder further up, air gets thinner
- weather + clouds occur in this layer
LAYERS OF THE ATMOSPHERE: stratosphere
- order
- features
2nd layer
- gets warmer
- contains ozone layer (absorbs harmful UV rays from sun)
- drier than troposphere
LAYERS OF THE ATMOSPHERE: mesosphere
- order
- features
3rd layer
- coldest layer
- meteors/rock fragments burn up on entry
LAYERS OF THE ATMOSPHERE: thermosphere
- order
- features
4th layer
- hottest layer
- auroras occur within the layer
- space shuttle orbits
LAYERS OF THE ATMOSPHERE: exosphere
- order
- features
5th final layer
- very thin
- made up of He and H
Describe the timeline of the atmosphere and how gas concentrations have changed over time.
EARTH FORMS (4.6 BYA)
- by volcanic activity
- very hot
- mostly CO2, with N2, some H2O + methane
EARTH COOLS
- H2O cools, forming oceans
- CO2 dissolved into oceans, taken in by organisms
- CO2 confined into sedimentary rock + FFs
PLANTS EVOLVE (2.7 BYA)
- Phs takes in more CO2, produces more O2
- other gases (methane, ammonia) reacted with O2, and decrease in quantity
- N is very stable, and has built up over time
NOW
- atmosphere mostly N2 (79%), O2, with small amounts of H2O, CO2, and other gases
State the types of evidence available for past climate change (9).
- provide some info on how they are used
Rock types + locations
- rocks in an area give info about past climates (e.g. ancient coral atolls in areas far from oceans)
Ancient landscapes (changes/structure)
- landscape shapes show climates of the past (e.g. U shaped valleys show the area was glaciated)
Fossils
- fossils indicate past climates by the organisms that lived there (e.g. ammonites found in a desert, coral found in a forest)
Sea/lake evidence
- changes in water lvls give an indication of past climate
Dendrochronology (tree rings)
- tree ring dating indicates whether a climate was wetter (rings are thicker)
Historical/archaeological records
- cave paintings may suggest species that the current climate would not support (e.g. grazing animals in Sahara)
Coral/sediment cores
- cores taken from coral/sediments show evidence for climate when they were formed, for 100s-1000s of years ago
- combined with fossils, can provide continuous data
Atmospheric monitoring
- baseline gas conc.s are monitored at: Tas (Sth Hemi), Hawaii (Nth Hemi)
- measure greenhouse/ozone depleting gases in clean air enviros
- critical for global monitoring
Ice cores
- very robust evidence
- cores drilled from ice caps
- past air is trapped in the ice from snow falling, this is analysed
- O2 indicates the temp of the past (less heavy O2 means cooler temps)
trade winds
- winds that circle the Earth near the equator
- EAST TO WEST (clockwise)
ENSO (El Nino Southern Oscillation)
- what?
- what is the graph that represents it
- predictable changes in atmospheric circulation (weather/wind/clouds) between North Australia and South America
- a cycle, around 4-7 years, from which weather predictions can be made
- known as a ‘climate driver’
- it oscillates between neutral, El Nino, La Nina
SOI (Sthn Osc Index) GRAPH
- gives an indication of development + intensity of El Nino/La Nina
- larger peaks show when cycle is in El Nino/La Nina
Describe the neutral phase of ENSO.
- what
- Walker Circulation
- in the phase more than 1/2 the time
- strong trade winds blow E to W
- causes upwelling of cold, nutrient dense water in Sth America (good for fishing)
WALKER CIRCULATION
- warm air over Nth Aus rises
- condensation/clouds causes rain
- dry air blows on T winds to Sth America
- gets cooler, descends
- is carried on T winds back to Aus
- gets warmer, cycle begins again
Describe the La Nina phase of ENSO.
- general effects
- Aus
- Sth America
- WALKER CIRCULATION INTENSIFIES - the ‘extreme’ version of neutral phase
- trade winds are stronger
- positive feedback loop (drives itself)
AUS
- warmer H2O in oceans in Nth Aus
- increased rainfall/clouds
- atmospheric instability: storms, cyclones, flooding
STH AMERICA
- colder H2O in oceans
- less rainfall, drought
- stronger upwelling (good for fisheries)
Describe the El Nino phase of ENSO.
- general effects
- Aus
- Sth America
- TRADE WINDS WEAKEN/REVERSE
- warm H2O drifts to Sth America
AUS
- colder H2O in oceans in Nth Aus
- less rainfall, drought, bushfires, heatwaves
STH AMERICA
- warmer H2O in oceans
- increased cloud/rain, flooding
- less upwelling (bad for fisheries)
biodiversity
the variety within all species and the ecosystems within they live
levels of biodiversity
- Genetic: differences among individuals/populations, due to sexual reproduction
- Species: the variety of different species within an ecosystem
- Ecosystem: all the communities, habitats and processes within different ecosystems
Explain the importance of biodiversity (3)
INTRINSIC VALUE
- everything has the right to exist
VALUE TO OTHER SPECIES/ECOSYSTEMS
- Genetics variation: increases resilience to change, increases chance of gaining useful adaptations
- Habitat variation: provides opportunities for competition, adaptation + evolution, conserving habitats preserves species/genetic diversity
HUMAN VALUE
- Economic benefits: wide variety of materials, wide gene pool reduces risk of diseases wiping out farmed products, warns us against use of some toxins (e.g. DDT), provides pharmaceutical services
- Ecosystem services: pollination, nutrient cycles, pest control via predators, maintain stable atmosphere (CR + Phs)