2.3 Weather processes and phenomena Flashcards
Adiabatic lapse rate
Change of temperature caused by the air changing internally. i.e rising and falling in height
Adiabatic processes
Change in temperature of a parcel of air caused by its ascent or descent. Changes are internal.
Advection fog
It is formed by warm air flowing over a cold surface, being chilled, reaching dew point , and condensation taking place, close to the ground’s surface.
Air mass
Large body of air with relatively similar temperature and humidity characteristics
Altitude
Measurement in height usually given in meters above sea level.
Clouds
Water vapour condensed into millions of minute water particles that float in masses in the atmosphere.
Condensation level
Altitude at which relative humidity is 100 percent, when clouds form.
Conditional instability
ask
When the ELR is lower than the DALR (dry adiabatic lapse rate) but higher than the SALR (saturated adiabatic lapse rate). The air in unstable so dew point is reached.
Depression
Region of low atmospheric pressure.
Dew
Precipitation in the form of moisture that collects on the ground.
How is dew formed?
It is formed after temperature of the ground has fallen below dew point of the air in contact with it.
Dew point
Temperature at which relative humidity is 100 percent
Environmental lapse rate (ELR)
Normal decline of temperature with altitude; usually about 6/1000m
Evaporation
Process by which a liquid if transformed into a gas.
Fog
Cloud at ground level, composed of water vapour that has condensed on particles of dust in the atmosphere.
Front
Boundary between a warm air mass and a cold air mass that results in frontal (cyclonic) rainfall
Humidity
Measure of the amount of moisture in the air.
Absolute humidity
How much moisture there is in the air
Relative humidity
How much moisture air at an specific temperature can hold
Instability
Refers to unstable atmospheric conditions (rising air) likely to cause cloud formation and precipitaion
Lapse rate
Rate of change of atmospheric factors (temperature and humidity) with changing altitude
Mist
Low cloud caused by condensation of water vapour in lower part of the atmosphere. (less thick than fog)
Orographic (relief) rainfall
Rainfall that occur when an airstream is forced to rise over a mountain range
Radiation fog
Fog forms on clear, calm nights when the land surface loses heat capacity the air above is cooled to below dew point and condensation takes place.
Rain shadow
Leeward side of hills, which has a relatively light rainfall compared to the windward side.
Stability
Refers to pressure conditions; air is unable to rise above a low level, calm , dry conditions.
Thunderstorm
Usually carried by intense heating of ground surface during the summer.
Dry adiabatic lapse rate (DALR)
Adiabatic cooling and warming in dry unsaturated air occurs at around 10/km
Saturated adiabatic lapse rate (SALR)
Air in which condensation is occurring. Between 4/km and 9/km