Air Mass
- 1000 km^2
How are air masses classified?
by temperature and humidity at source region
Atmospheric River
Sea Breeze
Land Breeze
Air humidity
Vapour Pressure
-share of air pressure made up by water vapour molecules at given T
Saturation
- air is in equilibrium with liquid
Saturated Vapour Pressure
Warm Tropical air SVP
- powers the tropical storms
Cold Polar SVP
- polar deserts created
Mixing Ratio
mass of water vapour per unit mass of dry air
specific humidity
mass of water vapour per unit mass of moist air
Max specific humidity means..
max water vapour per unit air mass
Relative humidity =
amount water vapour in air/max possible at given T *100
Dew Point
-temperature for air mass to become saturated
Condenstation Causes
- cooling of air
Diabatic
physical exchange of heat
Adiabatic
no physical exchange of heat
air stability
-temperature difference between inside air parcel and air surrounding parcel
Atmospheric Stability
-tendency of an air parcel to remain in place / change positions
Stable Atmosphere
-air resists upward displacement
Unstable Atmosphere
-air continues to rise until it reaches it’s own temperature and humidity conditions
Rising air causes
clouds and precipitation