Carbon and Water- Water Cycle Flashcards

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1
Q

What is a system?

A

A system describes the interrelationships (depend in each other) between living and non-living components within an environment such as a pond or forest. They generally are composed of inputs such as precipitation, stores such as water, outputs (processes) such as evaporation and photosynthesis is an example of a flow or transfer.
Systems help us understand the world around us and how energy is transferred between components of a system.

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2
Q

Define positive feedback. Use an example from a woodland to illustrate this.

A

A cyclical (circle) sequence of events that amplifies or increases change. Positive feedback loops exacerbate (increase) the outputs of a system, driving it in one direction and promoting environmental instability. E.G. Woodland carbon cycle - Increased temperatures due to climate change cause melting of permafrost. Trapped greenhouse gases are released, enhancing the greenhouse effect, raising temperatures further.

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3
Q

Outline how negative feed back can lead to falling temperatures

A

As it is a cyclical sequence of events that damp down the effects of a system. Increased surface temperatures lead to an increase in evaporation from the oceans. The leads to more cloud cover. Clouds reflect radiation from the sun, resulting in a slight cooling of surface temperatures.

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4
Q

Define dynamic equilibrium

A

This represents a state of balance within a constantly changing system

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5
Q

Explain how the water cycle can be closed

A

As an entirety (on Earth) it’s a closed system (only got flows and stores) as water is not lost to or gained from space

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6
Q

Explain how the water cycle can be open

A

At a local scale such as a drainage basin (area where water will flow into a river), it’s an open system. Precipitation is an input and runoff to the oceans is an output. There are many components and stores, such as trees, built-up areas and soil. Flows and transfers include throughflow (water moving underground) and groundwater flow.

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7
Q

Explain how the carbon cycle can be closed

A

The global carbon system is a closed system as there are no inputs or outputs in the system as a whole.

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8
Q

Explain how the carbon cycle can be open

A

At a local scale such as a forest, it is an open system with both inputs (processes) and outputs. There are many components and stores, such as rocks, the oceans and atmosphere. Flows and transfers include photosynthesis and respiration.

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9
Q

What are 4 characteristics of the global water cycle

A
  • water is not evenly distributed….
  • future wars may be over water….
  • ownership of water if a “hot” political issue. For example, damming rivers in one country can have serious repercussions for others.
  • 97.5% of water is saline (salty), and of the remaining 2.5% which is drinkable, half of it is stored as snow/ice…
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10
Q

What are the 4 main stores in the global water cycle

A
  • lithosphere (land)
  • atmosphere (air)
  • hydrosphere (liquid water)
  • cryosphere (frozen water - snow and ice)
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11
Q

What is an aquifer

A

An underground store of water

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12
Q

What aquifer dominates South America

A

Guarani aquifer dominates S.America

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13
Q

Explain the geological conditions needed for an aquifer to form

A

Permeable + porous rocks (chalk + sand stone)

Allow water through forming underground reservoirs

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14
Q

What is the upper layer of saturated rock called? Outline 2 reasons why this may rise or fall?

A

Water table. May rise or fall due to groundwater flow, water abstraction or recharge (water flowing into rock).

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15
Q

What is meant by a “fossil aquifer”

A

Desert aquifers formed 1000’s of years ago when climate was much wetter

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16
Q

Describe the distribution of aquifers (3)

A
  • found worldwide
  • not a lot in Asia
  • few found in Northern regions of the Northern hemisphere
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17
Q

How long does water remain in rivers

A

Rivers (2-6 months)

18
Q

How long does water remain deep down in the ground

A

Groundwater deep down (10,000 yrs)

19
Q

How long does water remain in lakes

A

Lakes (50-100 yrs)

20
Q

How long does water remain in the ground (not deep down)

A

Shallow G.water (100-200 yrs)

21
Q

How long does water remain in glaciers

A

Glacier (20-100 yrs)

22
Q

How long does water remain in the soil

A

Soil water (1-2 mths)

23
Q

Explain the high precipitation at the equator

A

It occurs due to the warm air rising and then as it rises it cools and condenses causing rainfall

24
Q

Why does the UK have variable rain & cloud cover?

A

Due to it being located in between the Polar and Ferrel Cells, these cells don’t mix so we have variable rain and cloud cover

25
Q

95% of water is locked up in which 2 ice sheets?

A

Antarctica and Greenland

26
Q

How old is the ice in Antarctica and Greenland

A

400,000 years

27
Q

What does “ice calving” mean?

A

Ice breaks away from an ice store

28
Q

“The equilibrium line in glaciers is moving to ever higher altitudes.” What does this mean?

A

This where the equilibrium line marks the altitude where annual accumulation and melting are equal. With climate change the line is moving to higher altitudes, making glaciers shrink and retreat.

29
Q

What is through flow

A

Through flow - Water flowing through soil towards a river channel.

30
Q

What is infiltration

A

Infiltration - Transfer morning of water from the ground surface into soil where it may then percolate into underlying rocks

31
Q

What is percolation

A

Percolation - Water soaking into rocks

32
Q

What is interception

A

Interception - Water intercepted and stored on leaves of plants

33
Q

What is evapotranspiration

A

Evapotranspiration - The combined losses of moisture through transpiration and evaporation

34
Q

Which water store has the shortest residence time? Suggest one reason for this

A

Interception as it is still exposed to the elements (e.g. wind blowing it off)

35
Q

Why does groundwater have the longest residence time?

A

Because it has no where to run off to it can it can only evaporate

36
Q

Explain 2 ways in which humans can increase overland flow

A

Deforestation removes vegetation stored, reducing outputs such as transpiration, increasing overland flow. Urbanisation may prevent infiltration, causing more groundwater + overland flow

37
Q

Account for 1 climatological factor in altering stores in a hillside system.

A

Storms - intense rainfall increases amount reaching the ground, increasing the magnitude of storms

38
Q

What is the drainage basin hydrological cycle

A

This is basically a detailed version of the water cycle. It is also very similar to the hillslope water cycle.

The hydrological cycle describes the continuous movement of water above and below the ground within a drainage basin. The water can appear in various forms and the cycle has no beginning or end. Within a drainage basin, it may be viewed as an open system with inputs, outputs, stores & transfers/flows.

39
Q

Using examples, illustrate how soil those and rock type can affect the transfer and storage of water within a drainage basin

A

The rock type affects the storage and transfer because permeable rock means water can pass through it meaning more water stores and it has a lower runoff figure, but with impermeable rock water can’t pass through it so there is more transfer and runoff. If the soil is utilising the water there is less water as runoff so there is more storage than transfer

40
Q

Explain, using an example, how vegetation has an important impact on drainage basin systems

A

River Severn is a forest area unlike River Wye, study showed that the forest area had increased evapotranspiration rates, so less water flows into rivers

41
Q

What is a flood hydrograph

A

this is simply a graph that shows how quickly and by how much a rivers discharge (the volume of water in it) rises after a period of heavy rain. By drawing these we can make judgements in the characteristics of the basin in which the storm event has occurred

42
Q

Explain how changes in water storage in the East Anglian Fens has had implications for the carbon cycle

A

This occurs in dry weather (low water table) - Peatlands are thick deposits of decomposed vegetation which act as important carbon stores. Dry peat is frittle & vulnerable to erosion, which can form black clouds of peat (decayed vegetation) as wind whisks peat up into the air. The ignition of peat can release carbon reducing carbon stores. Releasing harmful carbon dioxide emissions into the atmosphere