Water Cycle and Water Insecurity EQ1 Flashcards

1
Q

The planting of trees in an area that has not been forested in recent times

A

Afforestation

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2
Q

A measure of the proportion of the incoming solar radiation that is reflected by the surface back into the atmosphere and space

A

Albedo

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3
Q

The normal, day-to-day discharge of the river fed by groundwater flow

A

Base flow

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4
Q

Water is stored in rivers, lakes and groundwater in liquid form

A

Blue water

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5
Q

The area of land drained by a river and its tributaries

A

Catchment

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6
Q

The flow of water in streams or rivers

A

Channel flow

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7
Q

The storage of water in streams or rivers

A

Channel storage

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8
Q

The change from a gas to a liquid

A

Condensation

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9
Q

Often associated with intense thunderstorms, which occur widely in areas with ground heating such as the Tropics and continental interiors.

A

Convectional rainfall

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10
Q

Areas of the Earth where water is frozen into snow or ice

A

Cryosphere

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11
Q

A period of sustained, moderately intensive rain; it is associated with the passage of depressions

A

Cyclonic rainfall

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12
Q

The cutting down and removal of all or most of the trees in a forested area

A

Deforestation

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13
Q

The temperature at which dew forms; it is a measure of atmospheric moisture

A

Dew point

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14
Q

The conversion of water to vapour, as a result of the sun’s heating and air movement The change in state of water from a liquid to a gas

A

Evaporation

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15
Q

The combined effect of evaporation and transpiration

A

Evapotranspiration

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16
Q

The part of a storm hydrograph in which the discharge starts to decrease

A

Falling (recessional) limb

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17
Q

The rate of flow between the stores

A

Fluxes

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18
Q

Ancient, deep groundwater from former pluvial (wetter) periods

A

Fossil Water

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19
Q

Water stored in the soil and vegetation

A

Green water

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20
Q

The slow transfer of percolated water underground through pervious or porous rocks

A

Groundwater flow

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21
Q

The movement of water from the ground surface into the soil

A

Infiltration

22
Q

The maximum rate at which rain can be absorbed by a soil

A

Infiltration capacity

23
Q

Where water is captured by vegetation, or buildings and hard surfaces, before reaching the soil

A

Interception

24
Q

Water retained by plant surfaces and later evaporated or absorbed by the vegetation and transpired

A

Interception loss

25
Q

The time between peak rainfall and peak discharge

A

Lag time

26
Q

Concentrated on the windward slopes and summits of mountains

A

Orographic rainfall

27
Q

The time when the river reaches its highest flow

A

Peak discharge

28
Q

The transfer of water from the soil into the bedrock beneath

A

Percolation

29
Q

Lines of concentrated water flow between soil horizons to the river channel

A

Percolines

30
Q

The water loss that would occur if there was an unlimited supply of water in the soil for use by vegetation

A

Potential Evapotranspiration

31
Q

The movement of water in any form from the atmosphere to the ground

A

Precipitation

32
Q

The physical mechanisms that drive the fluxes of water between the stores

A

Processes

33
Q

A dry area on the leeward side of a mountainous area (away from the wind). The mountains block the passage of rain-producing weather systems and cast a “shadow” of dryness behind them.

A

Rain shadow

34
Q

Planting trees in places with recent tree cover, replacing lost primary forests

A

Reforestation

35
Q

The average time a water molecule will spend in a reservoir or store

A

Residence time

36
Q

The part of a storm hydrograph in which the discharge starts to rise

A

Rising limb

37
Q

The annual variation in discharge or flow of a river at a particular point or gauging station, usually measured in cumecs

A

River regime

38
Q

The upward movement of the water table into the evaporation zone

A

Saturated overland flow

39
Q

Water held within the soil

A

Soil moisture storage

40
Q

This is when water trickles along twigs and branches and then down the trunk

A

Stem flow

41
Q

Stocks where water is held, such as the oceans, lakes etc.

A

Stores

42
Q

The variation of discharge within a short period of time, usually in response to a period of rainfall

A

Storm hydrograph

43
Q

The movement of water that is unconfined by a channel across the surface of the ground. Also known as overland flow

A

Surface run-off

44
Q

Any surface water in lakes, ponds, puddles

A

Surface storage

45
Q

These approaches study the hydrological phenomena by looking at the balance of inputs and outputs, and how water is moved by stores and flows

A

Systems approach

46
Q

When the rainfall persists or is relatively intense and the water drops from the leaves, twigs, needles etc.

A

Throughfall

47
Q

The lateral transfer of water down slope through the soil via natural pipes and percolines

A

Throughflow

48
Q

The diffusion of water from vegetation into the atmosphere, involving a change from a gas to a liquid

A

Transpiration

49
Q

Any moisture taken up by vegetation and held within plants

A

Vegetation storage

50
Q

The balance between precipitation, evaporation and run-off (the difference between inputs and outputs)

A

Water budget

51
Q

The high land which divides and separates waters flowing to different rivers

A

Watershed