water and carbon cycle Flashcards

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1
Q

water can be stored in four areas?

A

hydrosphere, lithosphere, cryosphere, atmosphere

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2
Q

what is the cryosphere

A

any water that is frozen

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3
Q

what is the lithosphere?

A

water stored in the crust and upper mantle.

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4
Q

how much of earth’s fresh water is stored in the cryosphere and lithosphere store?

A

cryosphere- 69%

lithosphere- 30%

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5
Q

evaporation

A

when liquid changes state in to a gas

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6
Q

what affects the magnitude of evaporation.

A

it is dependent on season and location, as large levels of solar radiation combined with a large supply of water and warm dry air.

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7
Q

condensation

A

when water vapour changes state to a liquid. happens when the air cools to its dew point. e.g at night.

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8
Q

what affects the magnitude of condensation

A

amount of water vapour in the atmosphere and the temperature.

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9
Q

cloud formation

A

clouds form when warm air cools down, causing the water vapour In it to condense into water droplets, which gather as clouds.

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10
Q

what causes warm air to cool

A

topography, convection, other air masses.

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11
Q

topography

A

when warm air meets mountains, its forced to rise, causing it to cool. This results in orographic precipitation.

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12
Q

convection

A

when the sun heats up the ground, moisture on the ground evaporates and rises up in a column of warm air. as it gets higher it cools, resulting in precipitation.

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13
Q

other air masses

A

warm air is less dense than cool air. as a result when the two contrasting airs meet, the warm air is forced above the cool air. As this warm air rises it cools down causing frontal precipitation.

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14
Q

what is a drainage basin?

A

is the area surrounding the river where the rain falling on the land flows into that river. they are OPEN systems.

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15
Q

watershed

A

the watershed is the dividing ridge, any precipitation falling beyond the water shed enters a different drainage basin.

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16
Q

where can be water be stored on a local scale ?

A

interception,
vegetation storage,
surface storage,
groundwater storage,
soil storage.

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17
Q

what are the flows in the water cycle?

A

infiltration,
overland flow,
through fall,
stemflow,
through flow,
percolation,
groundwater flow,
baseflow,
interflow,
channel flow.

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18
Q

overland flow

A

water flowing over the land because of saturated soil.

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19
Q

through fall

A

water dropping from one leaf to another.

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20
Q

Throughflow

A

water moving slowly downhill through the soil.

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21
Q

percolation

A

water seeping down through the soil into the water table.

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22
Q

baseflow

A

groundwater flow that feeds into river banks and beds.

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23
Q

what are the inputs into the water system?

A

evaporation,
transpiration,
evapotranspiration.

24
Q

transpiration

A

evaporation from within leaves- plants and trees take up water through their roots and transport it to their leaves where it evaporates into the atmosphere.

25
Q

what is evapotranspiration?

A

the process of the two together.

26
Q

the water balance uk pattern

A
  • during wet seasons, precipitation exceed evapotranspiration. This creates a water surplus. the ground stores fill so that there’s more surface runoff and higher discharge, so river levels rise.

-in drier seasons these stores deplete as they are used and not replaced by further precipitation .

-therefore at the end of the dry season there’s a defect of water in the ground.

27
Q

peak discharge

A

discharge is the volume of water that flows in a river per second.

28
Q

lag time

A

this is the delay between peak rainfall and peak discharge, this delay happens because it takes time for water to enter the river.

29
Q

what affects the hydrographic shape?

A

size of drainage basins - larger basins have a higher peak discharge and longer lag times because more water can be stored and it takes longer to enter the channel flow.

shape of drainage basin - if the basin is largely circular it is more likely to be a flashy hydrograph because all points on the watershed are roughly the same distance from the point of discharge measurement.

ground steepness- shortens lag time and increases runoff.

rock type and soil type- increases peak discharge and shortens lag time.

30
Q

physical changes to the water cycle:

A

seasonal changes,
storm events,
el nino and la nina.

31
Q

human changes to the water cycle

A

farming practices,
land use change,
water abstraction,

32
Q

seasonal changes (water)

A

in the UK the size of inputs, flows and stores in the water cycle varies with the seasons:

  • water can freeze
  • seasonal vegetation can die/grow
33
Q

el nino and la nina

A

reduced precipitation in these regions leads to lower terrestrial moisture content, so there is less water in the soil available to evaporate. These regional reductions are so intense that they severely affect the global average volume of evapotranspiration

34
Q

farming practices

A
  • ploughing the soil increases infiltration.
  • arable farming can increase interception and evapotranspiration.
    -pastoral farming compacts soil, reducing infiltration and increasing run of as the compress the ground.
35
Q

land use change

A
  • deforestation reduces interception and evapotranspiration.
  • construction reduces infiltration and increases runoff.
36
Q

water abstraction

A
  • obviously reduces water in surface stores and ground stores.
    -increases during dry seasons and overall the abstraction is greater then the level of input.
37
Q

lithosphere (carbon)

A

over 99.9% of the carbon on earth is stores in sedimentary rocks.

38
Q

biosphere (carbon)

A

carbon is stored in the tissues of living organisms it is transferred to the soil when they decay.

39
Q

the carbon cycle

A

the carbon cycle is a closed system, there are inputs and outputs of energy however the amount of carbon always remains the same.

40
Q

carbon flows

A

photosynthesis,
respiration,
combustion,
decomposition,
carbon sequestration,
weathering,
ocean uptake and loss.

41
Q

photosynthesis

A

c02 + water -> light energy= glucose and oxygen.

42
Q

respiration

A

opposite to photosynthesis when animals convert oxygen and glucose into c02 and water. plants respire at night as there is no light energy.

43
Q

combustion

A

when fossil fuels are consumed or organic matter such as trees are burnt, they emit C02.

44
Q

decomposition

A

when organisms die they are broken down by decomposers such as fungi or bacteria- releasing c02 and methane. some carbon is transferred back to the soil in the form of humus.

45
Q

carbon sequestration

A

carbon from the atmosphere can be sequestered in sedimentary rock or fossil fuels.

carbon capture storage- captures 90% of the co2 produced but is extremely expensive.

46
Q

weathering

A

chemical weathering occurs when carbon reacts with water vapour to form acidic rain. this rain hits rocks and begins to dissolve them. the molecules from this reaction may be passed through the water cycle and enter the oceans, here they reacts with co2 from the sea to form calcium carbonate which assists in forming shells.

47
Q

ocean uptake and loss

A

co2 is directly dissolved from the atmosphere into the ocean. additionally when it is taken up by organisms such as plankton.

carbon is also transferred back to the atmosphere when water from deep in the oceans rises to the surface.

48
Q

types of carbon flows

A

fast carbon flows quickly transfer the carbon between sources, it takes a matter of minutes to days.
ph, resp, comb, decomposition.

sequestration is a slow carbon flow as it takes place over millions of years.

49
Q

changes to the carbon cycle (physical)

A

wildfires- co2 released through combustion. loss of vegetation so less evapotranspiration. fires can encourage growth log term.

volcanic activity- carbon stored within the earth in magma is released during eruptions.
in 1815 MT Tambora in Indonesia produced sulphur dioxide gas which blocked solar radiation reducing global temperatures by 0.4-0.7 degrees celsius in 1816

50
Q

human changes to the carbon cycle

A

hydrocarbon extraction/ use,
deforestation,
farming practices- pastoral and arable farming. rice paddies emit methane.
land use changes- concrete production releases co2.

51
Q

the carbon budget

A

the carbon budget is the balance between inputs and outputs to a store at any scale or the balance of exchanges between the four major stores.

carbon source - a store that emit more carbon than it absorbs.
carbon sink- the opposite.

52
Q

the carbon cycle affects the atmosphere and climate

A

affects the amount of gases containing carbon in the atmosphere.
the enhanced greenhouse affect- the greenhouse gases trap solar radiation causing global warming.
change in temperature can cause events such as storms.

53
Q

the carbon cycle affects the land

A

warmer temps melt permafrost and release greenhouse gases within them. can also increase frequency and intensity of fires.

54
Q

the carbon cycle affects the oceans

A
  • increased levels of co2 in the atmosphere can increase the acidity of the oceans because the oceans absorb more co2.
  • global warming can also affect oceans, e.g. organisms such as phytoplankton that is sensitive to temp may die.
  • warmer water is less able to absorb co2 .
55
Q

links between water and carbon

A

-carbon combines with water to form chemical weathering.

-water is needed for photosynthesis, which removes carbon from the atmosphere.

-the amount of co2 in the atmosphere affects global temperatures, which affect the amount of evaporation that can take place.

56
Q

climate change affects life on earth

A
  • the pattern of precipitation is said to worsen.
  • increased frequency of extreme weather events.
    -agricultural productivity will decrease.
  • sea levels expected to rise further.
57
Q

human intervention of climate change.

A

individual - change in habits or installation of sustainable energy production e.g solar panels.

national- governments can reduce the cost of renewable energy sources. they can also invest in ccs.

global- the 2015 Paris agreement, countries limited the amount of emissions. also carbon trading schemes where businesses are limited on the emissions they can produce.