Pressure Gradient Force
the movement of air from an area of high pressure to an area of low pressure
Convergence
the movement of air coming together; occurring at lows
Divergence
the movement of air moving apart; occurring at highs
Coriolis Effect
apparent force (rotation, doesn’t need anything to prompt it, it just is), dependent on latitude
Friction
real force (stationary, needs something to act upon it to be realized), interrupts winds at the surface due to textures
Geostrophic Wind
air aloft in the atmosphere only influenced by PGF and Coriolis
Dynamic
Occurs due to mechanical movement
Thermal
Occurs due to thermodynamic forces
High pressure
any pressure higher than 1013 mb
Low pressure
any pressure lower than 1013 mb
Dynamic high pressure
a high pressure created by shear force, not thermodynamic
Dynamic low pressure
a low pressure created by shear force, not thermodynamic
Thermal high pressure
a high pressure area
Thermal low pressure
a low pressure area
PAUSE: DRAW THE GLOBAL PRESSURE SYSTEMS
PICTURE:
Poles: Thermal Highs
60°: Dynamic Lows
30°: Dynamic Highs
Equator: Thermal Low
International Convergence Zone (ITCZ)
areas of persistent cloudiness where trade winds converge; aka doldrums
Hadley cell
linked areas of rising and descending air in relation to the subtropical high and the Equatorial low
Polar cell
linked areas of rising and descending air in relation to the Polar high and subpolar lows
all winds aloft are…
westerlies
Ferrell cell
a hypothetical open cell that does not move due to thermodynamics, occurring in the space between the Polar and Hadley cells
Shear force
a force that slides against another
jet stream
currents of fast moving air occurring aloft in the mid-latitudes that influence surface pressure and pressure gradients
polar front jet stream
the jet stream occurring on the edge of the polar cell (~45°-60°)
sub-tropical jet stream
the jet stream occurring on the edge of the Hadley cell (~60°)