WorksheetsMETEOROLOGY AND NATURAL PURIFICATION PROCESSES
Total questions: 15
Worksheet time: 11mins
An interaction of four elemental properties of atmosphere: heat, pressure, wind and moisture.
SCALES OF MOTION
Lapse Rate
Plume Types
Circulation pattern developed under influence of regional or local topography that occur on scales of hundreds kilometres.
Mesoscale
Microscale
Macroscale
Comes from sun as short-wave radiation in the form of visible light.
Pressure
Heat
Wind
Heat transfer by direct physical contact of air and earth .
Convection
Evaporation-condensation
Conduction
Process initiated by the rising of warm air and the sinking of cold air
Convection Current
Evaporation-condensation
Conduction
Defined as the rate at which air temperature changes with height that varies widely depending on location and time of day
(a)
Condensation releases latent heat in the parcel, thus the cooling rate of the parcel slows, so called _____.
DRY ADIABATIC LAPSE RATE
WET ADIABATIC LAPSE RATE
LAPSE RATE
It is determined by the temperature difference between an air parcel and the air surrounding
LAPSE RATE
INVERSION
ATMOSPHERIC STABILITY
A condition when the environmental lapse rate is less than the adiabatic lapse rate (cools at less than 9.8°C/1000 m)
STABLE CONDITION
UNSTABLE CONDITION
NEUTRAL CONDITION
It is important as the dividing line between stable and unstable conditions. It is when the environmental lapse rate is the same as the dry adiabatic lapse rate.
UNSTABLE CONDITION
NEUTRAL CONDITION
STABLE CONDITION
It occurs when air temperature increases with altitude.
Inversions
Lapse Rate
Atmospheric Stability
A type of plume where stream of pollutant undergoes rapid mixing.
CONING PLUME
FUMIGATING PLUME
LOOPING PLUME
Related to clear skies, light winds, and stable atm. It reflect the relative uniformity of air masses.
LOW-PRESSURE SYSTEM
HIGH-PRESSURE SYSTEM
NORMAL SYSTEM
It describes the transport and diffusion of a gas (or particle) from a source to a receptor according to stability class and other parameterized characteristics of the atmosphere.
GAUSSIAN DISPERSION
GAUSSIAN INVERSION
GAUSSIAN DIFFUSION
Type of plume created when atmospheric conditions (inversion layer) are stable above the plume and unstable below (superadiabatic).
CONING PLUME
FUMIGATING PLUME
LOOPING PLUME
