Air Currents Flashcards
How many properties of air circulate in the atmosphere
4 Air Density, Capacity to contain water vapor, Response to change in pressure, Production of heat when water vapor condenses from gas to liquid
Air Density 1
The mass of molecules in the air in a given volume
The mass of molecules in the air in a given volume
The density of air determines its movements
Less dense air rises whereas denser air sinks
Warm air has a lower density than cold air so it
rises
Capacity to contain water vapor 2
Warm air isn’t just denser than cold air it has a higher capacity for water vapor
Higher precipitation means it will be
More humid
Response to change in pressure 3
As air rises the pressure decreases
What happens when temperature falls
Saturation point decreases, water condenses into liquid clouds and precipitation forms
Production of heat when water vapor condenses from heat to liquid 4
Water vapor in the atmosphere condenses into liquid water, energy is released as heat, which leads to latent heat release
A major contributor of different climates is
Atmospheric convection currents
How is the Intertropical Convergence Zone (ITCZ) formed
The circulation of Hadley Cells is driven by the intense solar energy that strikes the earth near the equator which causes ascending branches of the two Haley cells to converge and form ITCZ
ITCZ characterized by
Dense clouds and intense thunderstorm activity
Saturation Point
The maximum amount of water vapor in the air at a given tempature
Adiabatic cooling
The cooling effect of reduced preesure on air as it rises higher in the atmosphere and expands
Latent heat release
The release of energy when water vapor in the atmosphere condenses into liquid water