Exam 2 Chap8 Flashcards
This exist whenever air pressure varies between locations
it also can be measured in direction of greatest change
also travels perpendicular to isobars
air pressure gradient
there are two types horizontal (more common) and vertical pressure gradient
What happens with closely spaced isobars?
air pressure changes rapidly with distance
strong pressure gradient
stronger winds blows from high to low pressure
What happens with widely spaced isobars?
air pressure changes gradually with distance
weaker pressure gradient
high pressure at the bottom but low at the top, will blow slower than closely spaced isobars
What is the centripetal force?
Center seeking force,
affects winds on a curved path
force directed perpendicular to direction of object’s motion, toward center of circular orbit
Relevant for winds that are blowing on a curved path
What is the coriolis effect ?
not a true force but an effect, apparent deflected motion of object to the right northern hemisphere
stronger at the poles, weakest at the equator
influences the wind in large scale weather systems
This is resistance an object as it moves in contact with another object or medium
friction happens in the boundary layer in the atmosphere
it slows down winds closer to the earth’s surface
creates turbulence
force that holds objects to the earth’s surface
Gravity only influences ascending or descending air
hydrostatic equiplibrium is ?
the balance between the force of gravity pulling an air parcel down towards the earths surface vs. the vertical pressure gradient that wants to pull the air parcel up in the atmosphere; these two forces are balanced so the air parcel stays right where it is
horizontal movement of air (No curvature here) that follows a straight path at altitudes above the atmospheric boundary layer (away from the earth’s surface where there is frictions)
the geostrophic Wind
Geostrophic wind also
wants winds to blow from high pressure to low pressure
there are two things at play the coriolis effect and the horizontal pressure gradient…
HPG wants the air parcel to go up but the coriolis pulls the movement to the right the longer the trajectory the longer the coriolis effect is going to be.
When both reach equilibrium the air parcel will be parallel to the isobars
This wind is similar to the geostrophic wind in that it is up out of the boundary layer and no friction is coming in to play. this time we are looking at a curved path so another force kicks in which is the centripetal force..
Gradient wind it occurs around high and low pressure centers above the boundary layer…moves counterclock wise in the northern hemisphere —
What are surface winds like
friction combines with the coriolis effect to balance the horizontal pressure gradient force….friction acts directly opposite the wind direction. The coriolis effect always at the right angle to wind direction .
-Winds cross isobars at an angle that depends on roughness of earth’s surface
High pressure cell surface winds
clockwise and out in the northern hemisphere
decreases as it moves out
-anti cylone
low pressure cell surface winds
counter- clockwise and in northern hemisphere
wind moving in this direction are defected to the right (c effect)
-cyclone
Forces change with altitude
the closer to earths surface the winds are, the more friction comes into play
for the same horizontal air pressure gradient the angle between the wind direction and isobars decrease with altitude in the atmospheric boundary layer.