Ch 4 Flashcards
First 10 miles closest to Earth
Troposphere
Above troposphere (10-31 mi)
Stratosphere
3 primary reasons to unequal heating
Angle at which sun’s rays strike earth, variation in amount of surface area, and some areas reflect more light than others
Reflectivity of a surface
Albedo
Max amount of water possible in air
Saturation point
Caused by change in pressure when air rises or sinks
Adiabatic heating/cooling
Happens when water vapor condenses, becomes liquid, and heat is released
Latent heat release
Global air movement patterns initiated by unequal heating
Convection currents
Circulation of convection currents
Hadley cells
Area of Earth that receives most intense sunlight
Intertropical convergence zone (ITCZ)
Deflection of an object’s path that occurs Bc of earth’s rotation
Coriolis effect
Large-scale water patterns circulating clock-wise in northern hemisphere, counter-clockwise in Southern Hemisphere (surface currents)
Gyres
Upward movement of deep waters
Upwelling
Driven by water that is usually salty
Thermohaline Circulation
Happens when warm ocean currents heat up continents
Heat Transport