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54 Cards in this Set
- Front
- Back
Atmosphere |
Transparent gases surrounding the Earth |
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Weather |
Short-term conditions of the atmosphere |
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Climate |
Long-term average condition of the atmosphere |
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Energy budget |
Amount of energy entering, leaving and transferring within the system |
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Diurnal |
24hr period (day and night) |
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Insolation |
Incoming solar radiation |
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Albedo |
Reflected solar radiation |
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Sensible heat transfer |
Transfer of heat from one area to another |
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Long-wave radiation |
Energy radiating from the Earth to space |
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Latent heat transfer |
Loss or gain of heat (result of condensation or evaporation) |
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Sub-surface supply |
Heat transferred to soil/ rock in the day being released to the atmosphere at night |
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Global energy budget |
Whole planet’s energy system |
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Net radiation balance equation |
(Incoming solar radiation + atmospheric counter radiation) - (reflected solar radiation + outgoing terrestrial radiation) |
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Terrestrial radiation |
Long-wave radiation which is given off |
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Atmospheric counter-radiation |
Long-wave radiation emitted from the earth to the atmosphere after it absorbed the short-wave radiation |
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Short-wave radiation |
Energy radiating from the sun to earth |
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Outgoing terrestrial radiation |
Radiation from the atmosphere/ Earth |
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Diurnal range |
Temperature difference between night and day |
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Thermohaline circulation |
Heat transferred through the ocean |
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Coriolis force |
Spinning of the Earth |
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Low pressure |
Air rising |
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High pressure |
Air sinking |
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Equatorial low pressure belt |
The zone where warm air near the equator rises |
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Trade wind |
Air/ wind returning to the equator |
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Sub-tropical high pressure belt |
Area where air descends in the tropics of cancer and Capricorn |
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Temperate low pressure belt |
Areas near the poles where air rises |
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Absolute humidity |
Water vapour measured in grams per cubic metre (g/m3) |
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Relative humidity |
Amount of water vapour in the air at a given temperature compared to how much it can hold at that temperature |
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Specific humidity |
Water vapour in the atmosphere measured in kg |
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Humidity |
How much water vapour is in a parcel of air at any given time |
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Dew point |
When a change in temp or pressure forms precipitation |
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Condensation nuclei |
Water droplets forming around pollen or dust particles |
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Sublimation |
Water vapour <-> solid form |
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Specific humidity |
Water vapour in the atmosphere measured in kg |
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Humidity |
How much water vapour is in a parcel of air at any given time |
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Dew point |
When a change in temp or pressure forms precipitation |
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Condensation nuclei |
Water droplets forming around pollen or dust particles |
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Sublimation |
Water vapour <-> solid form |
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Environmental lapse rate |
Expected decrease in temp as height rises |
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Environmental lapse rate |
Expected decrease in temp as height rises |
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Adiabatic lapse rate |
What actually occurs as air rises |
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Environmental lapse rate |
Expected decrease in temp as height rises |
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Adiabatic lapse rate |
What actually occurs as air rises |
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Dry ALR |
The rate of air cooling or warming when condensation doesn’t occur |
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Environmental lapse rate |
Expected decrease in temp as height rises |
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Adiabatic lapse rate |
What actually occurs as air rises |
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Dry ALR |
The rate of air cooling or warming when condensation doesn’t occur |
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Saturated ALR |
Rate of air cooling at dew point and condensation occurring |
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Atmospheric stability |
Air rising and cooling at quicker rate than air surrounding it |
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Atmospheric stability |
Air rising and cooling at quicker rate than air surrounding it |
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Atmospheric instability |
Air rising and cooling slower than its surrounding, continuously rising |
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Atmospheric stability |
Air rising and cooling at quicker rate than air surrounding it |
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Atmospheric instability |
Air rising and cooling slower than its surrounding, continuously rising |
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Conditional instability |
Cool air being forced to rise continuously |