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Latitude
horizontal lines showing distance from the equator
Albedo
the amount of light reflected off an object
Altitude
Height above se level in the air
Elevation
height above the sea level on land
Humidity
the amount of water vapor in the air
Damp soil
wet sediments with water in the interstitial spaces
Wind
horizontal movement of air
High air pressure
high density air, air sinks so weight of the air increases, cold air
Low air pressure
low density air, air rises so the weight of the air decreases, warm air
Hadley Cells
convection cells divided up around 30 degrees North and South and 60 degrees North and South latitude
Prevailing winds
winds that
No wind Zones - why occurs
at 0, 30, 60 , 90 degrees because air is either rising or sinking not moving horizontally
Coriolis Effect
apparent deflection of global winds due to the rotation of the earth
Ocean current
Density current and surface currents
Surface ocean current
flow of water of similar characteristics that are pushed along the surface by winds
Density current
vertical flow along the bottom due to differences in density
subsurface ocean current
currents that flow under the top of the Ocean due to differences in density
Gyre
circular pattern
Counter current
two currents moving in opposite directions