unit 5, exam 2 Flashcards
forces that act on atmosphere
pressure gradient
coriolis
friction
geostrophic wind
forces are balanced
upper atmosphere
pressure gradient force and Coriolis balance each other out.
wind then flows perpendicular to isobars
going counter/clockwise within perspective hemisphere
gradient wind
geostrophic flow includes centripedal that maintains parallel flow around isobars
force
push or pull on an object with a vector quantity both in magnitude and direction
forces not balanced
near the surface friction slows, reduces the coriolis and allows pressure gradient forces to dominate which causes convergence in L pressures and divergence at H pressures
one cell model
hadley cell 18th century scientist proposal for trade winds single cell of air movement assumes: no land, sun directly over equator, no rotation
wind
the movement of air in response to temperature and pressure gradients
wind is light
pressure gradient is weak
widely spaced isobars
wind is sstrong
pressure gradient steep
closely spaced isobars
large gradient
fast winds
small gradient
slow winds
pressure gradient
change in air pressure over a distance
always present vertically(large gradient) and horizontally (much smaller gradient)
pressure gradient FORCE
a response to horizontal air pressure gradients, the wind blows form high pressure to low pressure, orienting perpendicular to isobars
H-pressure system
anticyclone, brings fair weather
L-pressure system
cyclone, brings stormy weather