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10 cards from this deck
Invisible gas in the atmosphere
Amount of moisture or water vapour present in the air
Proportion of water vapour to max capacity at given temp, as %
Air at 100% relative humidity, can't hold more water vapour
Warm air can hold much more water than cooler air
Temperature at which water vapour condenses into water droplets
Height above sea level where air reaches dew point & condenses
They form at same height where condensation begins
(Water vapour content / Water vapour capacity) × 100
Temperature (determines air's water vapour capacity)
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