Carbon And Water Cycles Flashcards

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1
Q

Within the boundaries of systems we find three properties

A

Elements- substances that make up the system
Attributes- characteristics of the elements perceived and measured
Relationships- how elements and attributes work together

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2
Q

Types of system

A

Close system- transfers of energy into and beyond system boundary but not matter
Open system- where matter and energy are transferred across the boundary
Isolated systems- no interactions with anything our side of the system, no inputs and outputs

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3
Q

Positive feedback loop

A

Seven cents in which before me an action causes a knock on affect/secondary affect. Becomes changed and often irreversible
E.g. Release of more water vapour

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4
Q

Negative feedback loop

A

A circumstance and which performing an action causes fewer performances of an action

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5
Q

Atmospheric water

A

Water found in the atmosphere; mainly water vapour with some liquid water and ice crystals. Water vapour found in visible masses (clouds)

In three states: gas (water vapour) being most
Important as it absorbs, reflects and scatters radiation
Small increase in water vapour- positive feedback loop

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6
Q

Cryospheric water

A

Water locked up on the Earth surface as ice

Permafrost
Alpine glaciers 
Sea ice
Ice caps
Ice sheets
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7
Q

Terrestrial water

A
Consists of 
surface water (rivers, lakes, wetlands)
groundwater
soil water
biological water (all water in biomass)
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8
Q

Oceanic water

A

Makes up 97% of water cycle
Salt dissolved in water stops freezing below 0
PH 8.5- increasing due to CO2 concentration

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9
Q

Factors affecting water flow and transfer

A
Evaporation (factors affecting the rate of reaction: insolation, surface area, temperature, humidity)
Condensation 
Precipitation 
Sublimation 
Desublimation
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10
Q

Changes in the magnitude of water cycles over time

A

Daily
Dew and condensation in the morning
More evaporation during day
Weather generally

Seasonally
More water in monsoon seasons
Ice coverage dependent on season

Long periods of time
Warm and cold periods (holocene, Pleistocene, ice age)- human activity and milankotvitch

This takes place on local, micro and global scales

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11
Q

What is a drainage basin

A

Area of land drained by a river and it’s tributaries, this includes water found below the water table as well as soil water and surface flow

  • Drainage basins separated by highlands called watershed
  • Drainage basins are cascading systems- all linked so input of one is output of another
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12
Q

What is a river regime?

A

The variability in its discharge throughout the course of the year in response to precipitation, temperature, evapotranspiration and drainage basin characteristics- displayed on a hydrograph

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13
Q

What is the water balance

A

Balance between inputs (precipitation) and outputs (run off)

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14
Q

Factors affecting water flow in drainage basin

A
Vegetation and land use
Soil type and depth 
Rainfall
Shape of the land 
Bedrock 
Climate 
Conditions in drainage basin (ground frozen/baked)
Size and shape of river
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15
Q

Recharge season

A

When precipitation exceeds potential evapotranspiration

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16
Q

Surplus season

A

When precipitation exceeds potential evapotranspiration

17
Q

Storm hydrograph

A

Graph used to show how a rivers discharge changes in response to a precipitation event
Precipitation- bar graph
River discharge- line/ coloured area

18
Q

Features of the storm hydrograph

A

Peak rainfall- hour of greatest rainfall
Peak discharge- time of maximum river discharge
Falling limb- a period of time when the rivers discharge is falling
Normal flow- base flow of the river
Rising limb- period of rising river discharge

19
Q

Physical factors affecting storm hydrograph

A
Drainage basin shape
Relief
Drainage density
Pervious weather conditions 
Geology
Vegetation type and cover 
Precipitation intensity 
Drainage basin size
20
Q

Human factors affecting the storm hydrograph

A
Deforestation 
Afforestation
Land use
Urbanisation 
Fluvial engineering 
Drainage basin management
21
Q

Where carbon stored?

A

Lithosphere-earths crust and upper mantle (organic and inorganic)
Hydrosphere- oceans (surface layer, intermediate and deep layer, living organic matter)
Biosphere- total sum of all living matter (living vegetation, plant litter, soil hummus, peat, animals)
Atmosphere- CO2

22
Q

Movement of carbon

A

Moves from each store in a continuous cycle- through transfers and fluxes
Net carbon sink- carbon entering a store then leaving
Net carbon source- leave and then enters

23
Q

Natural factors increasing atmospheric CO2

A
Forest fires
Volcanic eruptions 
Equestration of of carbon from the sea
Biomass shuts down (seasonal)
Interglacial periods
24
Q

Natural factors decreasing atmospheric CO2

A

Long term reduction of volcanic activity
Glacial periods
Biomass regrows

25
Q

Human factors increasing atmospheric CO2

A
Deforestation 
Climate change- burning CO2
Warmer oceans- less absorbed 
Combustion of forests 
Increased farming 
Tundra releasing carbon- due to climate change
26
Q

Human factors decreasing atmospheric CO2

A

Carbon capture schemes

Afforestation

27
Q

Impact of carbon on the land

A
Agriculture more intensive 
Increased temps
More wildfires 
Farmland replaced by trees
More CO2 in atmosphere means more plant growth
28
Q

Impact on the ocean

A
Ocean acidification 
Ocean warming
Melting sea ice 
Ocean salinity 
Sea level rise
29
Q

Impact on the atmosphere

A

20% of CO2 in atmosphere

Enhanced greenhouse effect (radiative affect)

30
Q

Change in the climate

A

Temp rise
Decrease in arctic and Antarctic
Increase in winter precipitation (N hemisphere)
Decrease in summer precipitation

31
Q

Individual human intervention in climate change

A

Turn off lights
Walk/ less car more public transport
Eating less meat
Insulate house

32
Q

Local/ regional human intervention in climate change

A

Other clean energy projects
Recycling projects
Greater public transport networks (other schemes-congestion charge)
Greener transport- electric cars, tax incentive

33
Q

Global

A

Summits: Rio 92, Kyoto 97, Paris 2015