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How is the troposphere heated
The troposphere is heated from the Earth by terrestrial radiation and conduction.
What is terrestrial radiation
The Earth absorbs the sun’s rays, heats up, and emits its own radiation.
Which gases absorb terrestrial radiation
CO₂ and H₂O vapour.
Does terrestrial heating increase or decrease with altitude
It decreases as radiation energy lessens.
Which heats faster: land or water
Land heats quicker.
Which cools faster: land or water
Land cools quicker.
What is conduction
Heat transfer through direct contact.
How does conduction heat the air
Air in contact with the surface heats or cools depending on the surface temperature.
How deep into the troposphere does conduction affect
The first 4000 feet.
How is heat distributed vertically through the troposphere
By convection, turbulent mixing, release of latent heat, compression, and advection.
What is convection
Air warmed by radiation or conduction becomes less dense and rises.
What causes air to stop rising in convection
When it cools, becomes denser, and sinks.
Does convection occur on small scales, large scales, or both
Both.
What is turbulent mixing
Wind blowing over rough terrain produces eddies that mix air vertically.
What is an eddy
A circular motion of air moving contrary to the main flow.
What causes latent heat release
Condensation occurring after water vapour reaches its dewpoint.
What does evaporation require
Heat absorption.
What does condensation release
Latent heat into the atmosphere.
How is heat transported upward by latent heat
Water vapour carries heat aloft before releasing it during condensation.
What is compression in the atmosphere
Subsiding air enters higher pressure and warms as it compresses.
What is subsidence
Descending air from higher altitudes.
Why does compressional heating occur
Same amount of air molecules in less space increases temperature.
What is advection
Horizontal transport of atmospheric properties such as air and moisture.
When does advectional warming occur
When cool air moves over a warmer surface.
How is the atmosphere cooled
Temperature decreases with height; nighttime radiational cooling; conduction cooling the lower 4000 feet.
What is the Environmental Lapse Rate (ELR)
The actual temperature decrease with altitude at a given time and place.
What is the average ELR
1.98°C per 1000 feet.
Why does the atmosphere cool at night
More radiation is emitted than absorbed.
What is expansional cooling
As air rises, pressure drops, air expands, and temperature decreases.
Why does rising air expand
Air pressure decreases with altitude.
Define adiabatic. Occurring without gain or loss of heat.
What happens to a gas compressed adiabatically
Its pressure and temperature increase without heat exchange.
What happens to a gas expanded adiabatically
Its pressure and temperature decrease without heat exchange.
What is adiabatic heating
Heating due to compression of descending air.
What is adiabatic cooling
Cooling due to expansion of rising air.
What is the Dry Adiabatic Lapse Rate (DALR)
3°C per 1000 feet.
When does air cool at the DALR
When it is unsaturated.
What happens when rising air reaches dewpoint
Condensation begins.
What effect does condensation have on temperature
Releases latent heat, reducing the rate of cooling.
What is the Saturated Adiabatic Lapse Rate (SALR)
1.5°C per 1000 feet.
Why is SALR lower than DALR
Latent heat released during condensation warms the air.
Name the six adiabatic cooling methods. Orographic lift, upslope lift, frontal lift, mechanical turbulence, convection, convergence.
What is orographic lift
Air forced upward over a mountain.
What is upslope lift
Air cools as it is lifted up gradually rising terrain.
What is frontal lift
Warm air being forced upward along a front.
How does warm air rise along a warm front
It slides up over retreating cold air.
How does warm air rise along a cold front
Cold advancing air undercuts warm air, forcing it upward.
How does mechanical turbulence cause cooling
Air is pushed upward by surface friction and expands/cools.
Why does convection cause cooling
Warmer surface areas cause buoyant rising air that expands/cools.
What is convergence
Surface winds flowing inward toward a low pressure center and rising.
What is stability
The tendency of an object to return to its original position if displaced.
What is stable air
Air that resists vertical motion.
What is unstable air
Air that promotes vertical motion.
What is neutral air
Air that neither resists nor promotes vertical motion.
What determines whether air rises or sinks
Its buoyancy compared to the surrounding air.
When is air more buoyant
When it is warmer (less dense) than the surrounding air.
When does unstable air stop rising
When it becomes the same temperature as surrounding air.
How do you determine atmospheric stability
Compare the lapse rate of rising air to the lapse rate of surrounding air.
What is the surrounding (non-rising) air lapse rate
2°C per 1000 feet (ICAO standard lapse rate).
What lapse rates must be compared for stability
ELR vs DALR or SALR.
If ELR is greater than DALR, is the air stable or unstable
Unstable. (Slide does not answer; aviation rule provided.)
If ELR is less than SALR, is the air stable or unstable
Stable. (Aviation answer added.)
If ELR is between DALR and SALR, what type of stability
Conditionally unstable. (Added question.)
What is the albedo effect
Darker surfaces absorb more solar radiation.
What type of surface has highest albedo
Fresh snow.
What type of surface has lowest albedo
Asphalt or dark soil.
What happens when winds converge at the center of a low
Air is forced upward, cools, and expands.
Which cooling method is responsible for most cloud formation
Adiabatic cooling.
Which lifting method is most common on windy days over rough terrain
Mechanical turbulence.
Which lifting method generates lenticular clouds
Orographic lift. (Added aviation knowledge)
What does convection typically create
Cumulus clouds.
Why does rising air cool
Decreasing pressure causes expansion.
Why does descending air warm
Increasing pressure causes compression.
What determines cloud base height
Temperature–dewpoint spread. (Added aviation knowledge)