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76 Terms

1
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What are open systems?

Have external inputs and outputs of energy and matter exchange at its boundaries

<p>Have external inputs and outputs of energy and matter exchange at its boundaries</p>
2
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What are closed systems

No inputs occur from outside and nothing is lost. Only energy as its input and output and matter is contained within system boundary

<p>No inputs occur from outside and nothing is lost. Only energy as its input and output and matter is contained within system boundary</p>
3
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What is the global hydrological system?

The continuous movement of water on above and below the Earths surface. It’s a closed system so no external inputs or outputs, no water lost or gained

4
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Explain how water is recycled in the global hydrological system

  1. The sun evaporates surface water into water vapour

  2. The water vapour condenses to form clouds

  3. Moisture is transported around the globe which drives atmospheric circulation and returns to surface as precipitation

  4. When water reaches the ground, some water will evaporate back into atmosphere whilst some water may percolate the ground to form groundwater.

5
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How does the hydrological cycle lead to local temperature fluctuations

Water evaporates using energy form its surrounding to do this process, which cools the environment. When water condenses, heat is released.

6
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How is gravitational potential energy involved in the hydrological system

When a water droplets falls from high above sea level to the ground it has a high amount of gravitational potential energy. When it’s in motion GPE turn into KE so allows water to move over the surface.

7
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What amount does freshwater make up in all of Earths water

2.5%

8
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What amount of freshwater is locked away and how

1.6% is locked away and 68.7% of this is locked away as ice within cryosphere and the remaining 30.1% is groundwater.

9
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How much of Earths freshwater is accessible to humans

1%

10
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Why’s water stored unevenly around the globe

Water is stored unevenly because of the uneven spread of land to sea and permeable or porous rock which enables aquifers to form.

11
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What are fluxes

Transfers of water in the hydrological cycle

12
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What are annual fluxes

Variations in flows due to to temperature, seasons and location. Flows like evaporation will be greatest in warmer areas so higher rates of precipitation. Store like ice caps will get smaller due to climate change but ocean stores will increase.

13
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What is global water budget

Difference between the inputs and outputs from the different stores

14
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What is residence times?

Time water is held in a store.

15
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What factors affect size of stores and water residence times

  • Flows or transfers like evaporation

  • Global factors like climate change

  • Local factors like human activity on a hill slope

16
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How do transfers affect size of water store and water residence time

More precipitation increases availability of water for storage. Or surface flow increases,allowing more infiltration.

17
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What’s cryosphere

Water stored in solid form like glaciers and ice sheets

18
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What’s hydrosphere

Water stored in liquid form like rivers and lakes, groundwater.

19
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How has climate change affected how water is stored

  1. During last ice age, third of earths surface was ice sheets and glaciers so increased cryosphere stores

  2. This reduced hydrospheres stone and sea levels where 100m lower.

20
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What’s the Inter tropical Convergence Zone

Area of low pressure that forms due to action of the Had,ey Cell, where the Northeast Trade Winds meets the Southeast Trade near the equator.

21
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Explain what happens at the Inter tropical convergence zone

The equator receives more insulation so higher temperatures which leads to more evaporation

Warm moist air rises, cools and condenses and forms banks of towering clouds with heavy rainfall

Low pressure zone created called ITCZ

22
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How is a positive feedback created when cryospheres melt

Melting of ice sheets adds water to hydrosphere like oceans. Ice shelves are destabilised so ice breaks off so they melt and hydrosphere store increases . This is positive feedback loop

23
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What are drainage basins

Area of land drained by a river and its tributaries with a boundary known as the watershed composing of hills and mountains. An open subsystem in hydrological system

24
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What’s a catchment area

An individual drainage basin is the area drained by a river and its tributaries

25
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What features do drainage basin features have

Watershed, source, confluence, tributary,mouth

26
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What’s confluence

Point where two rivers meet

27
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What’s tributary

A smaller stream or river flowing into a larger stream or river

28
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What’s the mouth and source of a river

Mouth- where river meets ocean or sea

Source-furthest point from mouth where river starts

29
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What is orographic(relief) rainfall

Warm moist air formed by evaporation and carried by prevailing wind is forced to rise over high ground like mountains. Air cools, condenses , forming clouds so leads to precipitation. In the rain shadow,Dry air descends and warms so more moisture held in atmosphere.

<p>Warm moist air formed by evaporation and carried by prevailing wind is forced to rise over high ground like mountains. Air cools, condenses , forming clouds so leads to precipitation. In the rain shadow,Dry air descends and warms so more moisture held in atmosphere.</p>
30
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What is a rain shadow

Region with little rainfall because it’s sheltered from prevailing winds by mountains

31
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What frontal rainfall

Warm and cold air masses meet and warm air rises over cold air. Warm air cools and condenses to form clouds creating precipitation.

<p>Warm and cold air masses meet and warm air rises over cold air. Warm air cools and condenses to form clouds creating precipitation.</p>
32
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What’s conventional rainfall

Ground heats air above it and moisture from ground evaporates. Warm moist air rises rapidly which cools,condenses to form clouds so that precipitation occurs.

<p>Ground heats air above it and moisture from ground evaporates. Warm moist air rises rapidly which cools,condenses to form clouds so that precipitation occurs.</p>
33
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What’s interception

Precipitation that doesn’t reach soil because it’s intercept by vegetation and the forest floor. Reduces surface runoff and so reduces soil erosion and flooding

34
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What’s infiltration

water on the ground soaking into the soil and porous rocks

35
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What’s throughflow

Flowing of water within soil moving towards the river

36
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What’s percolation

Movement of water through soil or underlying porous rocks

37
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What’s groundwater flow

Flow of water through rocks towards river

38
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What are the flows in a drainage basin

Throughflow, groundwater flow, infiltration,percolation, interception

39
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What is river discharge

Volume of water passing a point in the river channel at a hives unit of time and expressed as cubic metres per second or cumecs

40
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What are outputs of drainage basins

Evaporation, transpiration and channel flow

41
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How does climate affect drainage basins

  • It’s affect type and amount of precipitation

  • Extent of evaporation

  • Amount and type of vegetation

42
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How does soil affect drainage basins

  • Infiltration and through flow- the pores in soil affects rate of infiltration and through flow

  • Impermeable , saturated or compacted or frozen soil means low infiltration rates and high surface runoff

43
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How does vegetation affect drainage basins

  • Amount and type of vegetations affects interception, infiltration

  • Less or no vegetation means more surface runoff off and reduced interception and more infiltration

44
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How does geology affect drainage basins

  • Impermeable rocks reduces percolation so reduces groundwater flow

  • Geology affects type of soil which impacts flows

45
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How does relief affect drainage basins

  • Flatter slopes means more infiltration so reduces surface runoff off , steeper slopes means infiltration is reduced and surface runoff is increased

  • Upland areas experience more precipitation so affect flows in drainage basins

46
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How does deforestation impact drainage basins

Clearance of trees reduces interception and infiltration rates. Increases surface runoff o, reduces evapotrAnspiratipn which reduces precipitation

47
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How does urbanisation affect drainage basins

Tarmac and concrete are impermeable so reduce infiltration and increase surface runoff. Drainage system move water to rivers more rapidly so increases risk of flooding

48
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How does agriculture impact drainage basins

Reduces amount of large vegetation so decreases interception and increases runoff

49
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How does livestock farming impact drainage basins

Compaction of soil due to livestock trampling so soil is less porous so less permeable so reduces infiltration

50
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How does abstraction affect drainage basins

Over abstraction leads to reduced through flow and groundwater flow in river and reduces groundwater storage

51
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How do reservoirs affect drainage basins

Dams and reservoirs reduce water flow downstream. Increases evaporation as there’s greater surface area of water

52
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What are water budgets

Annual balance between inputs like rain and outputs like evaporation and their impacts on soil water availability

53
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What’s the water budget equation

Precipitation (P) = total runoff (O) + evapotranspiration(E)±changes in storages (S)

54
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How do west seasons impact water budget

Precipitation greater than evapotranspiration which creates water surplus. Groundwater stores fill with water which increases surface runoff o, higher discharge and higher river levels. So positive water balance

55
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How do drier seasons affect water budget

Evapotranspiration exceeds precipitation, plants absorb water so groundwater stores depleted so negative water balance

56
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What’s the soil water budget

Shows the balance between impure and outputs of a soil store over a year. Dependent on soil depth, type, texture, and permeability

57
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What is discharge

Volume of water moving past a point in a river per given time

58
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How is discharge calculated

Q(discharge in cumecs)= A(cross sectional area in m2) x V(velocity m/s)

59
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What factors influence discharge

Rate of precipitation snd how fast water transfers to the river across the drainage basin.

60
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What are hydrographs

Used to measure discharge and they can be annual or storm hydrographs

61
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What are annual hydrographs

Also called a rivers regime, shows the pattern of seasonal variation that takes places through a drainage basin to river discharge over a year. Measured in cumecs.

62
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What are storm hydrographs

Shows changes in a rivers discharge during and after a storm. Drawn to show a river reacts to a storm. They compare to variables, rainfall during storm in mm and river discharge in cumecs

63
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Describe the difference between how a flashy and a flat hydrograph is drawn

Flashy hydrographs have a short lag time with high peak discharge, steep rising limb. Flat hydrograph have longer lag time , low peak discharge and gentle rising limb.

<p>Flashy hydrographs have a short lag time with high peak discharge, steep rising limb. Flat hydrograph have longer lag time , low peak discharge and gentle rising limb.</p>
64
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How does rock type affect shape of hydrographs

  • Impermeable rocks decreases percolation and increases surface runoff so flashy hydropgraph

  • Permeable rocks allow percolation so lower surface runoff so flat hydrograph

65
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How does soil types affect shale of hydrographs

  • Clay soils means less infiltration sp increases surface runoff so flashy hydrographs

  • Sandy soils have a high infiltration rate so decreases surface runoff so flat hydrograph

66
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How does weather and climate affect shape of hydrograph

  • Heavy or prolonged rainfall and rapid snow melt exceeds soil capacity so increased surface runoff so flashy hydrographs

  • Steady rainfall and slow snow melt don’t exceed infiltration capacity of soil so flat hydrograph. High evaporation means less surface runoff off so flat shape

67
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How does antecedent conditions affects shape of hydrographs

  • Saturates soil so infiltration is low and surface runoff is greater so flashy shape

  • Unsaturated soils so infiltration is high and surface runoff is low so flat

68
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How does vegetation affect shape of hydrographs

Deciduous plants and trees means less interception in winter as they shed leaves so flashy

Trees means high levels of interception so flat

69
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How does drainage basin size affect shape of hydrographs

  • Smaller basins have steep rising limbs and short lag time as water reaches rivers more quickly

  • Large basins have longer lag times and gentle rising limbs as water takes longer to flow through basin

70
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How does deforestation affect shape of hydrographs

  • Deforestation reduces interception, urbanisation increases impermeable surfaces, agriculture increases compaction of soil so increases surface runoff off so flashy shapes

  • Afforestation increases interception so flat.

71
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What are droughts

Extended period of time when there’s below average rainfall

72
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What are meteorological droughts

Occurs when there’s a rainfall deficit and caused by changes in atmospheric circulation leading to lack of rain from short term or long term changes , lack of rainfall combined with high temperatures so increases evaporation

73
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What is agricultural drought

Water deficiency in soil leading to crop failure and reduced biomass

74
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What is hydrological droughts

Lack of water stored on surface and underground in lakes, rivers, reservoirs and aquifers

75
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What’s the El Niño Southern Oscillation(ENSO) cycle

Movement of warm water mass in the equatorial Pacific Ocean, due to changes in trade winds m atmospheric circulation and ocean currents. It includes phases El Niño and La Niña

76
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What’s the El Niño phase?

  • occurs when sea temp is 0.5 degrees above average so warmer average weather in eastern Pacific

  • Peaks usually in December and occurs 2-7 years

  • Can cause thermal expansion and sea level rise

<ul><li><p>occurs when sea temp is 0.5 degrees above average so warmer average weather in eastern Pacific </p></li><li><p>Peaks usually in December and occurs 2-7 years</p></li><li><p>Can cause thermal expansion and sea level rise</p></li></ul>