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NotesESSTopic 4.1Flows in the water cycle
Back to ESS Topics
4.1.46 min read

Flows in the water cycle

IB Environmental Systems and Societies • Unit 4

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Contents

  • The thirteen flows
  • Transfers and transformations
  • Evaporation, transpiration and evapotranspiration
  • How water vapour gets into the air
  • Drawing a systems diagram of the cycle
  • Exam-style question

Water moves between the stores by thirteen flows. Learn each one by what happens to the water.

FlowWhat happensYou can see it in
EvaporationLiquid water turns to vapour from seas, lakes, soilPuddles drying in the sun
TranspirationPlants release water vapour through their leavesA forest on a hot day
SublimationIce turns straight into vapour, skipping liquidSnow vanishing in dry wind
CondensationVapour cools and turns into dropletsClouds, dew, mist
AdvectionWind carries vapour or clouds sidewaysSea clouds blown inland
PrecipitationWater falls from cloudsRain, snow, hail
Melting / freezingIce turns to water / water turns to iceSpring snowmelt; a frozen lake
Surface run-offWater flows over the groundRain running down a road
InfiltrationWater enters the soilRain soaking into a lawn
PercolationWater moves down through soil and rockWater reaching an aquifer
StreamflowWater flows in a river channelThe Thames flowing to the sea
Groundwater flowWater moves slowly through rockA spring feeding a stream

The four the guide defines, and their neighbours

  • Sublimation: ice to vapour, with no liquid stage.
  • Advection: wind carrying vapour or clouds, for example from the sea over the land.
  • Infiltration: water entering the soil. Percolation: water moving down through it.
  • Surface run-off flows over the ground; streamflow flows in rivers.
  • Groundwater flow is slow movement through rock towards rivers and the sea.

Real example: near the top of Mount Everest, strong dry winds make snow on the summit ridge sublimate: it turns straight into vapour, so the snow vanishes without ever melting.

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Every flow is either a transformation, which changes the state of the water, or a transfer, which moves it to a new place.

The points to remember

  • A transformation changes the state of water: liquid, gas or solid.
  • Transformations: evaporation, transpiration, condensation, sublimation, melting, freezing.
  • A transfer moves water to a new place without changing its state.
  • Transfers: advection, precipitation, run-off, infiltration, percolation, streamflow, groundwater flow, plant uptake.
  • If the figure says evapotranspiration, write that word, not 'evaporation' or 'transpiration' alone.
Remember it as: Transformation changes its form; transfer changes its place.

Transformations (state changes)

  • Evaporation, transpiration
  • Condensation
  • Sublimation
  • Melting, freezing

Transfers (place changes)

  • Advection, precipitation
  • Run-off, streamflow
  • Infiltration, percolation
  • Groundwater flow, plant uptake

Real example: on the River Thames, rain soaking into the Cotswold hills is a transfer (infiltration), and the mist rising off the river on a cold morning comes from a transformation (evaporation then condensation).

Only the first answer counts: Give one transfer and one transformation, both from the figure. A wrong first answer is not rescued by a right second one.

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Evaporation and transpiration both put water vapour into the air, so they are often measured together as evapotranspiration.

The points to remember

  • Evaporation is from non-living surfaces: seas, lakes, wet soil.
  • Transpiration is from living plants, through stomata.
  • Evapotranspiration is the two together: the total loss of water vapour from an area.
  • It rises with heat, wind, dry air, more plants and more water available.
  • Animals lose water by sweating and breathing, but only plants transpire.

More evapotranspiration

  • Hot: puddles dry faster
  • Windy: washing dries faster
  • Dry air
  • Lots of plants
  • Plenty of water

Less evapotranspiration

  • Cold
  • Still air
  • Humid air: washing dries slowly
  • Few plants
  • Dry ground: nothing to lose

Real example: a single large oak tree can transpire over 400 litres of water on a hot summer day. In the Sahara, by contrast, evapotranspiration is tiny: the sun is strong, but there is almost no water to lose.

Another favourite question shows a figure with one way water enters the air, and asks for one more.

Ways water vapour enters the atmosphere

  • Evaporation from oceans, lakes, rivers and wet soil.
  • Transpiration (or evapotranspiration) from plants.
  • Sublimation from snow and ice.
  • Small amounts from respiration by animals and from burning fuels.
  • Pick one the figure does not already show.
Two panels: before clearance, rainfall, a thick evapotranspiration arrow, recycled rainfall and thin run-off; after clearance, thin evapotranspiration and thick run-off
Only evapotranspiration from trees is shown entering the air.

Real example: on this figure, evaporation from Sumatra's rivers or from the Indian Ocean would be a correct extra input: both put vapour into the air but neither is drawn.

Check it is not already there: If the figure already shows evapotranspiration, 'transpiration' repeats it. Choose evaporation from water or soil, or sublimation.

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The guide expects you to create a systems diagram of the water cycle and use it. Build it in five steps.

Five steps to draw it

  • Draw a box for each store: oceans, atmosphere, ice, lakes and rivers, soil, groundwater, plants.
  • Join them with arrows in the direction the water moves.
  • Write the process on every arrow, using the guide's names.
  • Mark which arrows are transformations (state changes) and which are transfers.
  • Check every box has at least one arrow in and one out: nothing is a dead end.
Systems diagram of the water cycle: eight stores in boxes joined by labelled arrows for evaporation, precipitation, advection, condensation, transpiration, snowfall, sublimation, melting, freezing, infiltration, plant uptake, percolation, run-off, streamflow and groundwater flow
A finished diagram: every store a box, every flow a labelled arrow.

Real example: to draw the River Severn's water cycle, start with boxes for the clouds over Wales, the soil, the groundwater and the Severn itself, then add arrows: precipitation, infiltration, percolation, groundwater flow and streamflow to the Bristol Channel.

Use it, too: Once drawn, the diagram answers questions: which flow did paving change? Which store is filling? Point to the arrow or box.
How this comes up: Paper 2, Section A: identify one transfer and one transformation on a water-cycle figure [2].
Systems diagram of the water cycle: eight stores in boxes joined by labelled arrows for evaporation, precipitation, advection, condensation, transpiration, snowfall, sublimation, melting, freezing, infiltration, plant uptake, percolation, run-off, streamflow and groundwater flow
Figure 1
IB-style questionIdentify[2 marks]

Figure 1 shows the water cycle as a systems diagram.

Identify one transfer and one transformation shown in Figure 1.

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On a hot day in Kew Gardens, London, water vapour rises from both the lake and the trees around it.

the difference between evaporation and transpiration.
[2 marks]

Related ESS Topics

Continue learning with these related topics from the same unit:

4.1.1What drives the water cycle
4.1.2The water cycle as a system
4.1.3Where the world's water is stored
4.1.5How human activities change water flows
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