1.2 Water Cycle Flashcards

1
Q

how many litres of water does the hydrosphere contain?

A

1.4 sextillion

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2
Q

how much water is freshwater

A

less than 3%

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3
Q

locations of the freshwater on earth

A

69% is frozen in the cryosphere
30% is groundwater
0.3% liquid freshwater in lakes and rivers
0.04% water vapour in the atmosphere

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4
Q

different states of water

A

solid
liquid
gas

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5
Q

solid to liquid

liquid to solid

A

melting

freezing

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6
Q

liquid to gas

gas to liquid

A

evaporation

condensation

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7
Q

gas to solid

solid to gas

A

deposition

sublimation

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8
Q

processes where energy is gained

A

melting
evaporation
sublimation

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9
Q

processes where energy is lost

A

freezing
condensation
deposition

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10
Q

Definition global hydrological cycle

A

water is continuously cycled between different stores

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11
Q

is the global hydrological cycle an open or closed system

A

closed no inputs or outputs of water

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12
Q

the amount of water present in each store varies over a range of scales from …. to ….

A

local to global

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13
Q

the magnitude of each store depends on the …. of water … … them

A

amount

flowing between

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14
Q

different flows occur at a range of … and … scales

A

spacial

temporal

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15
Q

4 ways the magnitude of stores varies over time and in space

A

evaporation
condensation
cloud formation and precipitation
cryospheric processes

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16
Q

magnitude of stores- evapouration

A

when liquid changes state to a gas, becoming water vapour. it gains energy from solar radiation,
evaporation increases the amount of water stores in the atmosphere.
magnitude of the evaporation flows varies by location and season
high- solar radiation, water, warm dry air
low- no solar radiation, little water, cool air that is already nearly saturated.

17
Q

magnitude of stores - condensation

A

water vapour changes state to become a liquid, loses energy to the surroundings, water vapour cools to its dew point.
decreases the amount of water stored in the atmosphere, when it condenses it forms dew on surfaces
magnitude of flows depends on the amount of water vapour in the atmosphere and the temperature, lots of water vapour rapid drop in temperature high condensation