Water And Carbon Flashcards
What is the water cycle
The flow of water between land, atmosphere and oceans through methods such as precipitation, evapotranspiration, run-off and ground water flow
What is the carbon cycle
Movement of carbon between atmosphere, oceans, sedimentary rocks, sea floor, soil and biomass, 99.9% of which is in sedimentary rocks. Flows between the stores include oxidation, combustion, respiration, photosynthesis and weathering
What is a closed system
No transfers of energy both into and beyond the system, so the global carbon or water cycle is a closed system
What is an open system
Systems that external input and output can be found, so the carbon and water cycle on a smaller scale are open systems
Inputs, outputs and stores of the water cycle
Stores- oceans 97%, polar ice/glaciers 2%, aquifers 0.7%, lakes, soils, atmosphere, rivers and biosphere containing 0.3% between them.
- water vapour evaporated from oceans inputs into atmosphere, vapour transpired through leaves and plants, together known as evapotranspiration
- moisture leaves atmosphere as precipitation and condensation glaciers release water by ablation
- run-off into rivers from land, rivers flow to oceans or lakes, infiltration through soil
- infiltration through soul, water under gravity may percolate into permeable rocks or aquifers, ground water eventually becomes run-off
Stores, inputs and outputs of carbon cycle
Stores- sedimentary rocks, atmosphere, oceans, fossil fuels, land plants, soil and sea floor sediment
Slow carbon cycle: carbon takes between 100-200 million years to transfer between each store, more about the transfer between the hydrosphere, lithosphere and atmosphere, most common is shellfish when they die their shells go to bottom of the ocean and in the heat, pressure and time they become carbon rich sedimentary rocks
Fast carbon cycle: 10-1000 times quicker, between life forms and the biosphere, land plants and microscopic phytoplankton key, photosynthesis they absorb CO2 from the atmosphere, respiration by plants and animals releases CO2, decomposition releases CO2
What is transpiration
Diffusion of water vapour to the atmosphere from leaf pores
How are clouds formed
- air warmed by contact with ground or sea rises as air rises and pressure falls it cools by expansion, known as convection
- air masses move horizontally across a cooler surface, advection
- warm air mixes with colder air
What is interception
Vegetation intercepts precipitation storing it on branches, leaves and stems, moisture is then evaporated or falls to the ground, throughfall, rainwater that flows down branches or stems is called stem flow
What happens to the ground in extended periods of rainfall
Soil becomes saturated and can’t store anymore water so has reached its infiltration capacity this means it becomes run-off or saturated overland flow
Precipitation impact in carbon cycle
CO2 dissolves in rainwater to form weak carbonic acid
Tundra case study basic facts
8 million km2 in Canada, Siberia and Alaska, negative heat balance for 9 months of the year, in winter 2 weeks no sun -40 degrees, low precipitation, lack of biodiversity and wildlife
Water cycle in tundra
50-350mm of annual precipitation (low)
Small stores of water in the atmosphere low temp = low humidity
Limited transpiration from lack of vegetation
Low rates of evaporation
Permafrost acts as barrier so small amounts of infiltration
Sharp increase in river flow early summer as active layer melts
Ponds and wetlands on tundra in summer as permafrost stops drainage in winter months
Carbon cycle in tundra
Contains globally 1600GT
Slow decomposition so more carbon accumulates
Carbon in tundra soil is 5 times larger
Used to be carbon sink but due to global warming becoming a carbon source
Physical factors affecting the water cycle
Temperature- below freezing so water stored as ground ice in permafrost layer. In summer thawing means water flows on the surface, lots of ponds. Poor drainage as permafrost stops infiltration.
Permeability- low owing to the permafrost and the rocks which dominate the geology in arctic