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54 Cards in this Set

  • Front
  • Back

Atmosphere

Transparent gases surrounding the Earth

Weather

Short-term conditions of the atmosphere

Climate

Long-term average condition of the atmosphere

Energy budget

Amount of energy entering, leaving and transferring within the system

Diurnal

24hr period (day and night)

Insolation

Incoming solar radiation

Albedo

Reflected solar radiation

Sensible heat transfer

Transfer of heat from one area to another

Long-wave radiation

Energy radiating from the Earth to space

Latent heat transfer

Loss or gain of heat (result of condensation or evaporation)

Sub-surface supply

Heat transferred to soil/ rock in the day being released to the atmosphere at night

Global energy budget

Whole planet’s energy system

Net radiation balance equation

(Incoming solar radiation + atmospheric counter radiation) - (reflected solar radiation + outgoing terrestrial radiation)

Terrestrial radiation

Long-wave radiation which is given off

Atmospheric counter-radiation

Long-wave radiation emitted from the earth to the atmosphere after it absorbed the short-wave radiation

Short-wave radiation

Energy radiating from the sun to earth

Outgoing terrestrial radiation

Radiation from the atmosphere/ Earth

Diurnal range

Temperature difference between night and day

Thermohaline circulation

Heat transferred through the ocean

Coriolis force

Spinning of the Earth

Low pressure

Air rising

High pressure

Air sinking

Equatorial low pressure belt

The zone where warm air near the equator rises

Trade wind

Air/ wind returning to the equator

Sub-tropical high pressure belt

Area where air descends in the tropics of cancer and Capricorn

Temperate low pressure belt

Areas near the poles where air rises

Absolute humidity

Water vapour measured in grams per cubic metre (g/m3)

Relative humidity

Amount of water vapour in the air at a given temperature compared to how much it can hold at that temperature

Specific humidity

Water vapour in the atmosphere measured in kg

Humidity

How much water vapour is in a parcel of air at any given time

Dew point

When a change in temp or pressure forms precipitation

Condensation nuclei

Water droplets forming around pollen or dust particles

Sublimation

Water vapour <-> solid form

Specific humidity

Water vapour in the atmosphere measured in kg

Humidity

How much water vapour is in a parcel of air at any given time

Dew point

When a change in temp or pressure forms precipitation

Condensation nuclei

Water droplets forming around pollen or dust particles

Sublimation

Water vapour <-> solid form

Environmental lapse rate

Expected decrease in temp as height rises

Environmental lapse rate

Expected decrease in temp as height rises

Adiabatic lapse rate

What actually occurs as air rises

Environmental lapse rate

Expected decrease in temp as height rises

Adiabatic lapse rate

What actually occurs as air rises

Dry ALR

The rate of air cooling or warming when condensation doesn’t occur

Environmental lapse rate

Expected decrease in temp as height rises

Adiabatic lapse rate

What actually occurs as air rises

Dry ALR

The rate of air cooling or warming when condensation doesn’t occur

Saturated ALR

Rate of air cooling at dew point and condensation occurring

Atmospheric stability

Air rising and cooling at quicker rate than air surrounding it

Atmospheric stability

Air rising and cooling at quicker rate than air surrounding it

Atmospheric instability

Air rising and cooling slower than its surrounding, continuously rising

Atmospheric stability

Air rising and cooling at quicker rate than air surrounding it

Atmospheric instability

Air rising and cooling slower than its surrounding, continuously rising

Conditional instability

Cool air being forced to rise continuously