Topic 5 - EQ1 - Water (Miss M) Flashcards

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1
Q

What is the order of the biggest water stores on earth?

A

Oceans then cryosphere then terrestrial then atmosphere

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2
Q

What are fluxes?

A

Measurements of the rate of flow between stores

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3
Q

What are processes?

A

The physical mechanisms such as evaporation that drive the flow of water between the stores

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4
Q

What is blue water?

A

Water stored in rivers, lakes, oceans, streams and groundwater (visible)

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5
Q

What is green water?

A

Water stored in the soil and vegetation (invisible)

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6
Q

In which store does water have the longest residence time in?

A

Cryosphere, followed by groundwater then oceans then other terrestrial stores (other than groundwater), finally the shortest RT is in the atmosphere (just 10 days)

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7
Q

What are the two types of energy that the Water cycle relies on? Why?

A
  • Solar energy is required to evaporate the water
  • Gravitational potential energy keeps the water moving around the atmosphere and around the system through inputs, outputs and flows
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8
Q

What is the global water budget?

A

The global annual balance of water flows and size of water stores

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9
Q

Is the water system considered a closed system?

A

Yes - because of this NASA estimates that every drop of freshwater has been consumed at least once before

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10
Q

What is evapotranspiration?

A

Evapotranspiration is the sum of evaporation from the land surface plus transpiration from plants

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11
Q

What percentage of the Earth’s water is freshwater?

A

2.5%

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12
Q

Where is the majority of freshwater stored?

A

Glaciers and ice caps, and ground water (glacial water is inaccessible)

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13
Q

What is the main source of water for humanity?

A

Rivers - the water in rivers is just 0.007% of total water on earth

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14
Q

Other than accessibility of usable water, what is the main other issue affecting the global usable water supply?

A

A rising population. The water cycle is closed and so the amount of water in the system stays stagnant, as the population increases the amount of water stays the same and with future overpopulation will come limited water availability.

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15
Q

What is the input into the drainage basin?

A

Precipitation

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16
Q

What are the 5 stores of water in the drainage basin?

A

Interception, surface storage, soil water storage, groundwater storage and Channel store

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17
Q

What are the 6 transfers of the drainage basin system?

A

Through flow (stem flow), infiltration, percolation, surface run-off, soil water through-flow, groundwater through-flow

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18
Q

What are the 3 outputs of the drainage basin system?

A

Evaporation, transpiration, river discharge

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19
Q

What is Convectional rainfall?

A

It is when the land becomes hot the air above expands and rises as it becomes warmer too, as the air rises it cools and its ability to hold water vapour decreases so condensation occurs and clouds develop. If the air continues to rise then rain will fall.

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20
Q

What is cyclonic rainfall (frontal rainfall)

A

When warm air (lighter and less dense) is forced to rise over cold, denser air causing water vapour to condense and form rain, because as warm air rises it cannot hold as much water vapour and so condensation occurs, clouds form and it rains

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21
Q

What is Orographic (relief) rainfall?

A

When air is forced to rise over a barrier, such as a mountain, it cools and condensation occurs causing rainfall concentrated on the windward slopes of the mountains or hills. Heavier rain on higher lands means that the downward slope is in a rain shadow and receives minimal rainfall.

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22
Q

Where is Convectional rainfall most common?

A

Tropical areas however it is sometimes seen in the South of the UK in summer

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23
Q

What rainfall do we see most in the UK?

A

Cyclonic rainfall

24
Q

What type of system is the Drainage Basin system?

A

The drainage basin is a subsystem within the global hydrological cycle. It is an open system as it has external inputs and outputs that causes the amount of water in the basin to vary over time. There are various inter-linkages between components of the system.

25
Q

How does interception cause variation within the drainage basin?

A

It delays the precipitation reaching the surface then reaching the river channel, increased lag time effectively

26
Q

What type of vegetation cover increases interception?

A

Denser types of vegetation, like coniferous forests

27
Q

What ‘type of precipitation’ is interception at its highest at?

A

Light rainfall of short periods (dry leaves and stems have the greatest water storage capacity)

28
Q

What is the main cause of secondary interception?

A

Coverage of shrubs and ground vegetation which catches rainfall from higher up trees/vegetation stopping water being drained.

29
Q

What diminishes interception greatly?

A
  • Deforesting land greatly diminishes interception in the drainage basin, unlike before there is nothing to stand in the way of precipitation and the surface.
  • The season of the year for deciduous trees, there is considerable less interception in areas with deciduous trees during autumn and winter as the trees have no leaves to catch precipitation
30
Q

What are the main things affecting the rate of infiltration?

A

Amount of water already in the soil (degree of saturation + water table level), vegetation cover, gradient of land and permeability of soil

31
Q

What is saturated overland flow?

A

Saturated overland flow happens when water accumulates in the soil until the water table reaches or ponds on the surface.

32
Q

What are the characteristics of the areas where saturated surface flow happens?

A

This particularly happens in areas of land with thin soils of moderate permeability

33
Q

What is infiltration excess surface flow

A

Infiltration-excess overland flow occurs when the rainfall intensity exceeds the infiltration capacity, so the excess water flows over the surface

34
Q

What helps increase the rate of soil throughflow?

A
  • A downwards gradient towards the river

- Low water table and little saturation so throughflow is not restricted

35
Q

What helps increase the rate of percolation?

A
  • No/little gradient so throughflow is not promoted as opposed to percolation
  • Permeable (porous and pervious) rocks
36
Q

What helps increase the rate of groundwater flow?

A
  • Rate of groundwater flow will also increase according to the angle of rock strata as gradient will increase speed of flow
  • Permeability of rocks (pervious and porous) to allow water to move through rocks
37
Q

What increases evaporation from the drainage basin?

A
  • Higher temperatures
  • Wind (Wind moving over a water or land surface can also carry away water vapor, essentially drying the air, which leads to increased evaporation rates)
38
Q

What increases transpiration in the drainage basin?

A
  • Wind (Wind will move the air around, with the result that the more saturated air close to the leaf is replaced by drier air)
  • More vegetation
  • More leaves (especially dark leaves
  • Soil moisture content (determines water available for transpiration)
  • More light intensity (stomata opens + more photosynthesis occurs)
39
Q

How can humans disrupt the Drainage basin?

A
  • Cloud seeding (dispersion of substances into the air to change the amount of precipitation, usually increase precipitation)
  • Deforestation (much less interception)
  • Using groundwater from aquifers quicker than water is replaced (greatly reduces groundwater flow and can cause rivers to run dry)
  • Urbanisation disrupts the interception store and infiltration transfer of the drainage basin because urbanisation creates impermeable surfaces that reduces infiltration and increases surface runoff and through-flow through man-made drains, this means the river discharge often increases rapidly and unnaturally
  • Dams and reservoirs disrupt the outputs of the drainage basin because the dam increases surface water stores which increases evaporation, this then reduces downstream river discharge
40
Q

What does a water budget reflect?

A

Water budget reflects the natural annual balance between inputs and outputs in a given river area which are influenced by climate. The balance determines the amount of moisture in soils.

41
Q

What is the formula for water budget?

A

The formula used is: Precipitation = channel discharge (water flow out of basin) + evapotranspiration +/- change in water storage. Whatever falls as precipitation should be balanced by the other components.

42
Q

What is field capacity?

A

Normal amount of water that can be held in the soil

43
Q

What is potential vs actual evapotranspiration.

A

The amount of water that could be lost by evapotranspiration if there was sufficient moisture available vs the amount of water that is actually lost through evapotranspiration

44
Q

What is soil moisture surplus?

A

When the soil moisture is full and there is excess water available for plants, runoff and recharge (Prec > Evapotranspiration)

45
Q

What is soil moisture utilisation?

A

Occurs when moisture from the soil stores is being used by vegetation/humans building a deficit as the precipitation rate is less than Evapotranspiration (Evapotranspiration > Prec)

46
Q

What is soil moisture recharge?

A

Occurs when moisture from precipitation infiltrates and percolates in the stores to relay the soil moisture utilisation deficit (Prec > Evapotranspiration)

47
Q

What is soil moisture deficit?

A

When there is not enough water left in the soil to match potential Evapotranspiration. Rivers run dry and drought ensues.

48
Q

What are the 6 main factors affecting a river regime?

A

Humans, precipitation, vegetation, temperature, size of the river and geology/soil

49
Q

How do humans affect river regime?

A

Man made dams regulate the flow of water which changes the discharge at times different to what would happen naturally

50
Q

How does precipitation affect river regimes?

A

Regimes often reflect rainfall seasons or when snow, or glaciers, melt in the spring-summer time

51
Q

How does temperature affect river regimes?

A

Warmer summer temperatures mean more evaporation which will be marked in the regimes

52
Q

How does the size of the river affect the river regime?

A

Larger rivers have more complex regimes because of varied catchments

53
Q

How does geology and soil affect river regimes?

A

Water is stored as groundwater in permeable rocks and is gradually released into the river as base flow, this tends to regulate the flow during dry periods

54
Q

What is a storm hydrograph?

A

A storm hydrograph is a graph showing variation in discharge (volume) of water in response to a rainfall event.

Shows response over a short period of time. Normally after an individual storm (few days).

55
Q

What are the factors that increase the probability of flooding?

A
  • Thin soil (low permeability and saturated quickly)
  • Steep relief (promotes surface run off not infiltration)
  • Human settlements with the laying of concrete and other impermeable surfaces
  • Impermeable rock layers (no percolation)
  • High intensity and prolonged rainfall
  • Deforestation (reduced infiltration and interception leading to possible saturated excess overland flow)
56
Q

Does urbanisation increase or decrease evapotranspiration? Why?

A

Decreases evapotranspiration, water runs off on the surface instead (see GoodNotes graphic pg31)