Humidity Flashcards
Freezing
Liquid to Solid
Absorbs Latent Heat
Freezing nuclei needed
Supercooled without nucleus to -50 before freezing
Supercool unstable
Condensation
Gas to liquid
Latent Heat released
Requires nucleus for water vapour
Psychrometer
Wet + Dry bulb
Wet cloth if evaporation occurs latent heat will be released causing variation in thermometers
Absolute Humidity
Amount of water vapour in volume of air (Mass)
G/m3
Vapour Pressure
Pressure from water vapour molecules
Humidity Mixing Ratio
Amount of water vapour in mass of dry air
Saturation
Max amount of water air can hold
Sublimation
Solid to gas
No nuclei needed
Latent heat released
Polar region terrestrial radiation
Deposition
Gas to solid
Latent heat absorbed
Nuclei required
Dew Point
Temp needed for saturation
Close temp = more likely for condensation and development of fog/cloud
Dry air has lower dew point
Warm air has higher dew point
Relative Humidity calculation
Amount of water in air/max water vapour air can hold x 100
Temp Effects on dew point
Increasing/decreasing temp on unsaturated air has no effect on dew point (Dew point can only be equal to or lower than the temp of air mass)
Decreased in saturated will condense and decrease dew point
Diurnal variation in humidity
Dawn/evening - Temp decrease mean higher relative humidity
Afternoon - temp increases lower relative humidity
Relative Humidity calculation from temp and dew point
100 - (temp-dew point) x 5
Neutral Stability
ELR = DALR in dry air
ELR = SALR for moist air