Water and Carbon Cycles: Systems Framework Flashcards

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1
Q

Define what a system is

A

A set of interrelated components working together towards some kind of process

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2
Q

What is an open system?

A

Matter and energy can enter and leave the system

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3
Q

What is a closed system?

A

Matter cannot leave the system, it can only cycle between stores, energy can enter and leave the system

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4
Q

What is dynamic equilibrium?

A

When there is disruption to one of the elements, so the other elements will change in order to return to a state of equilibrium, causing feedback loops

Disruptions:
Physical disruptions – storms or drought
Human disruptions – deforestation, urbanisation, water abstraction
Sudden disruptions may result in sudden change e.g. flooding

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5
Q

What is positive feedback?

A

The effects of an action are amplified or multiplied by subsequent secondary effects

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6
Q

What is negative feedback?

A

The effects of an action are nullified or reduced by subsequent secondary effects

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7
Q

What are elements?

A

A constituent part of the system

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8
Q

What is an attribute?

A

Characteristics of an element

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9
Q

What is a relationship?

A

the way in which the elements of a system interact

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10
Q

What are the inputs in the water cycle?

A

precipitation

matter and energy being added to the system

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11
Q

What are the outputs in the water cycle?

A

river discharge

matter or energy leaving the system

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12
Q

What are the stores in the water cycle?

A

ocean, groundwater, clouds

where matter or energy builds up

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13
Q

What are the flows in the water cycle?

A

channel flows

matter or energy moving from one store to another

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14
Q

What are the boundaries of the water cycle?

A

watershed

limits of the system

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15
Q

What is an example of a positive feedback loop?

A

Global temp rise -> warms oceans -> increased oceanic temperatures -> warm water is less able to dissolve gases -> dissolved CO2 is released by warmer oceans -> more CO2 back into atmosphere -> global temp rises

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16
Q

What is an example of a negative feedback loop?

A

burning fossil fuels increased atmospheric CO2 -> global temp increases -> more plant growth -> increased CO2 uptake by biosphere -> reduces atmospheric CO2 slowing rate of global temp increase

17
Q

What is a threshold?

A

A point in a condition or process that, once passed, triggers some kind of change

18
Q

Describe the varying sizes of global water stores

A
  • oceanic stores is the largest, 1.4 sextillion litres of water which is 97% of all the water in the hydrosphere
  • cryospheric store second largest (e.g. Ross Ice shelf or Greenland Ice sheets), 26 million km^3, contains 69% of freshwater (3% of all water is freshwater)
  • terrestrial water next, rivers take up 1 million squared km, largest being the Amazon River
  • biosphere second to last largest store, less than >1% of all freshwater, all living parts on the Earth
  • atmosphere is the smallest store, clouds, rain, vapour, ice crystals, a store 10 million% smaller than ocean
19
Q

Explain the sizes of the global water stores

A
  • Large stores have the longest residency times as the scale of processes is small relative to their size and they return the same amount (e.g. hydrosphere and evaporation/precipitation)
  • small stores have shorter residence times because the scale of the flows acting upon them are large relative to their size (e.g. atmosphere and evaporation/precipitation)
20
Q

Describe the flows between water stores

A
  1. Evaporation, increases amount of water stored in the atmosphere, liquid water changes state into a gas
  2. Condensation, vapour changes to liquid water, decreases water stored in the atmosphere
  3. Cryospheric Processes, including accumulation and ablation, changes amount of water stored in cryosphere
21
Q

What process are changing the size of the global water stores?

A
transpiration and respiration
plant uptake
percolation
groundwater flow
precipitation/condensation
evaporation
22
Q

What does the magnitude of each water store depend on?

A

The amount of water flowing between them

23
Q

What factors control the size of flows between water stores?

A
  1. evaporation = solar energy, supply of water, humidity of the air and temperature of air
  2. condensation = amount of water in atmosphere, solar radiation and condensation nuclei
  3. cryospheric processes = global climate
24
Q

What is the size of the largest water store?

A

Largest store is in the ocean with 1.3 million 1000km^3

25
Q

What is the size of the intermediate water stores?

A

Freshwater stores have intermediate sizes

- atmospheric water 2.7 (1000km^3) to cryosphere 26350 (1000km^3)

26
Q

What is the size of the smallest water store?

A

The smallest store is the atmosphere, over 10 million% smaller than the ocean store

27
Q

What is the largest flow of water stores?

A

Ocean evaporation and precipitation 413 1000km^3/year

28
Q

Q: Explain the role of cryospheric change in the water cycle [4 marks]

A
  • Cryospheric change has a regulatory role in sea levels
  • The cryosphere is a major store of water
  • In a period of cooling (glacial period) the cryosphere will grow in size
  • In a period of warming the cryosphere will add water to the cycle. As the water cycle restarts more of the ice melts and returns water to the sea
29
Q

What is a natural cause of variation in the water cycle?

A

Storm events transfer significant amounts of water from the atmosphere store to the hydrosphere and lithosphere stores.

30
Q

Outline an example of positive feedback feedback in the water cycle? [4 marks]

A
  • a system where the effects of an action are increased or
    amplified by its subsequent knock-on effects
  • Higher temperatures increase the melting of snow and ice
    leading to a reduction of surface albedo so more sunlight
    absorbed by land and sea. Temperatures increase further,
    which leads to further melting.
31
Q

Explain the concept of dynamic equilibrium in relation to the water cycle. [4 marks]

A
  • Dynamic equilibrium refers to the tendency towards a natural
    state of balance within the hydrological cycle
  • The cycle is a closed system as no water enters or leaves the system; it is simply recycled around the system
  • The dynamic equilibrium is easily upset by extreme events such as storms or droughts
  • Such events and processes cause sudden changes in the state of the system and disrupt or interfere with dynamic equilibrium as is the case with flooding