water and carbon cycles . Flashcards

1
Q

what are systems composed of ?

A

inputs - where energy or matter is added to the system
outputs - where energy or matter leaves the system
stores - where matter or energy builds up in a system
flows - where matter or energy moves in a system
boundaries - limits to the system ( eg. watershed )

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2
Q

what is dynamic equilibrium ?

A

when inputs equal outputs despite changing conditions

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3
Q

what is positive feedback ?

A

occurs when a chain of effects amplifies the impacts of the original event, leading to dynamic equilibrium

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4
Q

what is negative feedback ?

A

a chain of events the nullifies the impacts of the original event , leading to dynamic equilibrium

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5
Q

what are the inputs and outputs on a local drainage basin system ( local scale water cycle ) ?

A

inputs = precipitation
outputs = evapotranspiration ( from plants ), streamflow ( water flowing through streams into oceans and tributaries )

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6
Q

what are stores of a local drainage basin system ?

A

grounds water, soil water, rivers, interception, surface

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7
Q

what are flows in a local drainage basin system ?

A

infiltration, percolation, throughflow, surface runoff, groundwater flow, streamflow, stemflow

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8
Q

what is water balance ?

A

used to express the process of water storage and transfer in a drainage basin

calculated by : precipitation = total runoff + evapotranspiration +/- storage

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9
Q

what impacts the water cycle on a local scale ?

A

deforestation = less interception, soils less able to store water
storm events = increases runoff and water storage
seasonal changes = more interception in spring, snow reduces flows and hot weather reduces precipitation
agriculture - pastoral ground tramples so less infiltration, ploughing increases infiltration, ditches increase runoff
urbanisation = impermeable surfaces increase runoff

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10
Q

what is the soil water budget and how does it change throughout the year ?

A

shows the balance of inputs and outputs inn the water cycle and shows how inputs and outputs impact soil water storage and availability

there is a surplus of water in winter after recharge of soil water in autumn because there is more precipitation than evapotranspiration ( inputs exceed outputs )
in summer there can be a deficit of soil water as outputs exceed inputs

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11
Q

what is field capacity ?

A

maximum storage of water in soil

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12
Q

what does the water budget depend on ?

A

type, depth and permeability of soil and bedrock

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13
Q

what are the four areas water can be stored ?

A

hydrosphere - liquid water
lithosphere - stored in crust and upper mantle
cryosphere - frozen
atmosphere - water vapour

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14
Q

what are other ways water can be stored ?

A

aquifers - underground water stores, unevenly distributed worldwide. shallow groundwater aquifers can store water up to 20 years but deeper fossil aquifers may last up to 10,000 years
glaciers - store water 20-100 years
lakes - store wate 50- 100 years
seasonal snow cover and rivers - 2-6 months
soil water - 1-2 months

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15
Q

how does the water cycle change over time due to farming practices ?

A

ploughing breaks up the surface increasing infiltration, arable farming(crops) can increase interception and evapotranspiration, pastoral farming(animals) compacts the soil reducing infiltration and increasing runoff

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15
Q

how does the water cycle change over time through natural processes ?

A

in summer higher temperature = less precipitation, more evaporation, increased evapotranspiration(deciduous trees have leaves + high temp)

in winter = reduced flows as water stored as ice, reduced interception when deciduous trees loose leaves

15
Q

how does the water cycle change over time due to land use change ?

A

deforestation reduces interception, evapotranspiration but infiltration increases as land is clear
construction reduces infiltration and evapotranspiration but increases runoff

15
Q

how does the water cycle change over time due to water abstraction ?

A

volume of water in surface stores decreases
water abstraction increases in dry seasons as human demand is higher
water abstracted is often more than water inputted into aquifers = decline in global long term stores

16
Q

what is a flood hydrograph ?

A

used to represent rainfall for the drainage basin of a river and the discharge of the same river on a graph

16
Q

what are the two types of flood hydrogaphs ?

A

flashy = short lag time , steep rising and falling limb, higher flood risk , high peak discharge
subdued = long lag time, gradually rising and falling limb ,lower flood risk , lower peak discharge

17
Q

what would cause a flashy flood hydrograph ?

A

pastoral farming = ground trampled and compacted so less interception
deforestation = less interception
high rainfall intensity = higher discharge potential
antecedent rainfall = ground is saturated meaning increased surface runoff
impermeable underlying geology = decreased infiltration
high drainage density = many tributaries to the main river

18
Q

what are transfers of carbon on a local scale ?

A

photosynthesis - living organisms covert co2 into oxygen and glycose using light, they are sequestering carbon
respiration = releasing co2 and water from glucose and oxygen
plants are net carbon absorbers and net oxygen producers
decomposition, combustion

19
Q

what are the stores of carbon on the global scale ?

A

marine sediments and sedimentary rocks (lithosphere) - long term
oceans (hydrosphere) - dynamic
fossil fuel deposits (lithosphere) - long term but currently dynamic
soil organic matter (lithosphere) - mid term
atmosphere - dynamic
terrestrial plants ( biosphere) - mid term but very dynamic

20
Q

how does the carbon cycle change over time with natural processes ?

A

wildfires: transfer carbon from biosphere to atmosphere as co2 is released in burning, can encourage growth of plants in the long term
volcanic activity: carbon stored within the earth is released during volcanic eruptions

21
Q

how does the carbon cycle change over time through human practices ?

A

fossil fuel use - combustion releases co2 from the long term stores
deforestation - slash and burn techniques and stored carbon released
farming practices - arable farming releases co2 as animals respire, also ploughing can release co2 stored in the soil and farming machinery can release co2

21
Q

def carbon budget

A

the balance between carbon inputs and outputs to a store eg. atmosphere

21
Q

def carbon source

A

a store that emits more carbon than it absorbs

22
Q

def carbon sink

A

a store that absorbs more carbon than it emits

23
Q

what is the enhanced greenhouse effect

A

is the process causing global warming as high levels of greenhouse gases are being produced, these trap radiation from the sun

24
Q

what is the impact of the carbon cycle on tropical rainforests ?

A

high rates of photosynthesis and respiration in forests leads to greater humidity ,cloud cover and precipitation
deforestation reduces photosynthesis and respiration

25
Q

what is the impact of the carbon cycle on oceans ?

A

warmer oceans cause more plankton growth and plankton chemical production causing clouds to form

26
Q

what is positive feedback and e