Change in Magnitude of Water Stores (AQA A-Level Geography): Flashcards

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Change in Magnitude of Water Stores
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Water table

Boundary below which all gaps in soil/rock are filled with water

Transpiration

Loss of water from vegetation through stomata on leaf surfaces

Cold air vs warm air - water vapour capacity

Cold air holds much less water vapour than warm air

Effect of evaporation on surroundings

Cools surroundings (uses latent heat)

Condensation nuclei

Tiny particles (smoke, salt, dust) water molecules condense on

Dew point

Temperature at which air becomes saturated

Accumulation (cryospheric)

Build-up of ice mass

Drainage basin

Area of land supplying a river with water

Infiltration

Downward movement of water from surface into soil

Evapotranspiration

Total water output from drainage basin back to atmosphere

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