Meteorology 1 Flashcards
Standard Atmosphere
- Air is a perfectly dry gas
- MSL pressure of 29.92 inches of mercury
- MSL temperature of 15ºC
- Lapse rate of 1.98ºC/1000 ft
Principle Properties of the Atmosphere
- Expansion
- Compression
- Mobility
Sources of Moisture in Atmosphere
- Evaporation from oceans and lakes
- Transpiration from vegetation
Heating Processes - Conduction
- Heating through contact
- Air is poor conductor so limited in effect
Heating Processes - Convection
- Air that is warmed becomes less dense and tends to rise
- Rising continues until density (temp) is same as surrounding air
Heating Processes - Turbulent Mixing
- Friction causes eddies to form as air moves over surfaces
- Disruption is proportionate to terrain (rough terrain = more mixing)
- Can rise high into troposphere when combined with convection
Heating Processes - Advection
- Horizontal movement of air masses
- If it travels over a warm surface, the air mass will be warmed
Heating Processes - Compression
- Descending (subsiding) air increases in pressure, in turn increasing temperature
- Can occur along ridges of high pressure or over mountain ranges
- Known as adiabatic heating
Heating Processes - Release of Latent Heat
Changing state down an energy level releases heat energy and vice versa
Cooling Processes - Expansion Cooling
- Rising air expands, which causes a decrease in temperature (adiabatic cooling)
- Dry or saturated adiabatic lapse rate
Cooling Processes - Orographic and Upslope Lift
- Air flowing over topographical features causing it to rise
- Slope of terrain not important
Cooling Processes - Frontal Lift
Expansion cooling when warm air is forced up along a frontal surface
Cooling Processes - Mechanical Turbulence
Friction causes eddies to form as air moves over surfaces
Cooling Processes - Convection
Rising air cools according to the appropriate lapse rate
Cooling Processes - Convergence
Air at the centre of a low pressure area rises, causing cooling