Carbon and Water Flashcards
How much carbon is held in the hydrosphere ?
40,000 GTC
How is carbon from lithosphere transferred to the atmosphere ?
Natural gas gauses release carbon into the atmosphere and volcanoes do too
- when peat stored become oxygenated they release C into atmosphere
How much carbon is held in peat stores ?
700 billion tonnes
How is C stored in atmosphere ?
Mainly as CO2 which lasts 12 years
How are the carbon stored distributed across the world ?
Unevenly distributed
Terrestrial carbon cycle ?
Rock exposed after glacial retreat, so vulnerable to weathering
- rock exposed and broken down
- vegetation can grow on rock
- vegetation e.g lichen grows on rocks
- soil develops as organic matter is added to rocks
- wildlife becomes abundant
End serial stage = climatic climax e.g UK deciduous woodland
Main transfers in the carbon cycle ?
- Photo synthesis
- respiration
- decomposition
- combustion
- burial and compaction
- carbon sequestration
- carbon capture and storage
- weathering
Causes of change in the carbon cycle by human ?
- fossil fuel combustion (IPCC says 90% anthropogenic carbon release comes from this
- fossil fuels burnt for energy from rocks 85millions years old = global warming = melting cryosphere= positive feedback loop
- fertilisers and ploughing = main sources of agricultural emissions and fert washed into water ways
- US cattle accounts for 20% their total Meghan emissions
- 13 million hectares of land deforested each year and burnt = transferring carbon
- 200km squared of forest lost a day between 1980 and 2008
- urbanisation blocks sequestration
Physical causes of change in carbon cycle ?
- climate fluctuating between glacial and interglacial periods where carbon mirrors temperature. Increased temp = more carbon = positive feedback loop
- volcanoes return carbon to atmosphere that’s been kept in lithosphere for millions of years up to 380 million tonnes of CO2 a year compared to 30billion by humans
- wildfires convert huge carbon sinks into carbon sources
Impacts of cold climate on carbon cycle
- decomposers less effective so carbon transfer to soils and atmosphere reduced
- less sediment build up on ocean floor due to rivers being frozen up
- soils frozen over stopping transfer of peat carbon
- forest coverage changes
Impacts of warm conditions of carbon cycle
- Melting permafrost and tundra regions such as Siberia = pos feedback loop as carbon and methane released from permafrost enhance greenhouse effect
How does deforestation affect water cycle ?
- burning trees means carbon in ash form and leaching nutrients can be washed away by rainwater into streams killing fish = eutrophication
- no trees= no evapotranspiration
- less trees means more rain hits ground immediately compacting the ground and increasing overland flow, soil leaching takes place taking nutrients out of the soil and eutrophication
- more solid exposed to the sun = v dry and vulnerable to erosion
- no evapotranspiration means less water returned to atmosphere = change in magnitude of water stores and suppressing precipitation
Carbon budget ?
Uses data to describe the amount of carbon that’s stored and transferred within the carbon cycle
How much has the global temp increased since 1880 ?
.8 DC
Regional impacts of deforestation?
- dense veg regions have high respiration’s and photosynthesis= high humidity levels and more cloud coverage which affects regionals temps and rainfall
- no veg = arid dry region with less precipitation
Proliferation of plankton (absorb CO2) promotes formation of clouds through formation of chemical DMS
Volcanoes release CO2 and ash with other gases that absorb incoming solar radiation creating a regional cooling effect on the earth
Impacts of C cycle on land ?
Responsible for formation of soils and provides structure to the soil
- valuable source of energy through fossil fuels
Impacts of C cycle on ocean ?
- C can be converted into C carbonate which is used by some marine animals to make shells
- impacts in presence of proliferation of plankton where it is a common food in many food chains and passes along carbon
Impacts of carbon cycle on atmosphere ?
- helps warm atmosphere which was essential for life evolving in earth
What’s C role in supporting life ?
- 18% humans mass
- 50% trees mass
- essential for photosynthesis to create carbohydrates
- changes in magnitude of stored have huge implications for flora and fauna
Role of water in supporting life ?
- needed for drinking and irrigation
- spruce of power and energy
Positive feedback loop in water cycle ? And implications
Ice reflects suns radiation
- less heat is absorbed by the ice
- Arctic ice sheet been shrinking recently
- exposes more after to suns heat = warmer water = more ice melting
= economic and political implications as affects trading routes and exploitation of resources
Positive feedback loop in carbon cycle ?
- higher temps melt permafrost particularly in Siberia, amount of C held in permafrost = to the amount of C held in atmosphere, melting permafrost allows Oxygen to decompose C in PF releasing CO2 In has bubbles that rises to the surface and into the atmosphere
Key connection between carbon and water cycle ?
Natural unpolluted rain water is slightly acidic due to the presence of 3 substances and particularly C in troposphere
- if air is polluted with sulphur dioxide from combustion of fossil fuels = v acidic water e.g 1982 1.8 PH fog in west coast USA
Acid rain creates chemical weathering and breaks down rocks e.g chalk into calcium bicarbonate which is soluble. sSome C is returned to atmosphere and some to the hydrosphere by streams increasing magnitude of ocean C store
Water/ carbon cycle feedback
- phytoplankton lives in water and absorbs the C in it to photosynthesise
- marine phytoplankton releases chemical substance DMS which may promote the formation of clouds by blocking out solar radiation = global cooling and less sunshine = less phytoplankton growth = reducing cooling effect = negative feedback loop
Mountain thermostats ?
Research in Peruvian mountains shows mountainous areas help maintain global temps
- warmer climate = faster deeper root growth
- enables carbonic acid to reach carbonates therefore increasing weathering
- sequestration C from atmosphere for weathering = global cooling and less root growth
- self regulating and helps maintain global temperature balance
Ways of mitigating impacts of climate change ?
- Carbon capture and storage
- plantation forests (recommended by IPCC)
- modifying deforestation (FSC products )
International gov agreements
- Paris agreement (limit average global temp increase to 1.5DC above pre-industrial levels
Gov policies
- e.g Brazil protecting reserves in Amazon and reducing deforestation by 70%
Characteristics of tropical rainforests
- rich biodiversity
- in ITCZ
- annual rainfall = 2000+ mm
- emits 28% worlds oxygen
Precipitation in the TR cycle ?
Precipitation often V high and forms torrential down pours
- forest canopy intercepts 75% of rainfall (half of this is used in evapotranspiration)
- 25% rainfall is evaporated