Air Pressure
and Winds
- Chapter 6
- Pressure gradients
make the winds blow.
- Below is a review
of air pressure. In
class, we’ll start at the slide titled
“Wind.”
Air Pressure
Review
- Air Pressure: the
weight of the air above
- Thus, air pressure
decreases as height above sea level increases
- You can also think of air pressure as a force exerted against a surface by the continuous collision of gas
molecules
- The gas molecules collide with you from all directions, so therefore, you can think of air pressure as being
exerted in all directions
Air Pressure
Review
- Remember pressure
is related to temperature and volume (pV
= nRT)
- pV ~ T; p ~ T / V
- Also, density is
mass / volume
- So p ~ T * density
- Both the temp and
the density of the gas determine the pressure a gas will exert
Air Pressure
Review
- Cooler temps would
lower pressure if density remained the same
- But in the
atmosphere, cooler temps often result in greater density, which would
increase pressure
- A change in one of
the three variables causes changes in one or both of the others
- So it depends on
which change dominates as to what the conditions become
- Many times, the
density dominates, so a cold air mass from Canada
usually has higher pressure since it is so dense
Air Pressure
Review--Fig. 6-3
Air Pressure
Review
- Air Pressure
changes much more rapidly when one moves vertically in the atmosphere
than when one moves horizontally
- Then why does the
wind blow horizontally (North, South, East, West) and not vertically?
- Let’s
find out!
Air Pressure
Review—Fig. 6-7
Wind
- Wind is the result
of differences in air pressure over a distance—pressure
__________
- Air flows from
areas of _______ pressure to areas of _______ pressure
- ______ is
nature’s attempt to balance inequalities in air pressure
Wind
- Pressure
differences are usually generated by unequal ________ of
Earth’s surface
- So _______ ___________
is the ultimate energy source for most wind
Wind
- Air would flow
directly from high to low pressure in a straight path if the Earth did
not rotate and there was no friction
- However, since the
Earth does rotate, and there is friction between the air and the
ground, wind is controlled by a combination of forces
Wind
- The horizontal
movement of air is controlled by a ________ between forces that include
- The
Pressure-Gradient Force
- The _________
Force
- The Frictional
Force
PGF
- Pressure-Gradient
Force (PGF)
- Whenever we have a
____________ pressure gradient present, air is subjected to greater
pressure on one side than on another
- The _______
pressure side exerts a net force (the PGF)
on the air to push it from ______ to ______ pressure
PGF
- The greater the
difference between the high pressure area and low pressure area over
the same distance, the ________ the pressure gradient and PGF
- The greater the PGF, the _______ the air is
going to flow from ______ to ______ pressure (________ wind speeds)
PGF—Fig.
6-9
Sea Breeze
Example—Fig. 6-11
Vertical
Pressure Gradient
- There also exists a vertical pressure gradient force, which is much stronger, since pressure changes
more rapidly vertically than horizontally
- The vertical PGF wants to make
the air flow from the surface up to space (from higher to lower
pressure)
- However, gravity
acts against it, trying to pull air toward the surface
Vertical
Pressure Gradient
- In general in the atmosphere,
gravity and the vertical PGF are balanced--no ____ upward or downward flow
- When there are
______-scale upward or downward motions they are usually very slow
(less than 1 mile per day)
- Only
________-scale motions are rapid, like thunderstorm updrafts and
downdrafts
Coriolis Force
- Coriolis Force:
the force describing the ___________ of free-moving objects (including
wind) due to Earth’s __________
Coriolis Force
Coriolis Force—Fig. 6-13
Coriolis Force—Overhead Projector
Coriolis Force
- We saw how
north-to-south flow is deflected, but what about west-to-east?
- It’s
still deflected to the ______ in the NH
- Coriolis force
does depend on _________
- The deflection is
________ toward the poles and is ________ at the equator
Coriolis Force—Fig. 6-13
Coriolis Force--See Fig. 6-13
- Notice also that
the faster the object is moving, the greater distance it will be
deflected
- This happens
because faster winds cover a greater distance than slower winds in the
same time period
Coriolis Force
- For atmospheric
motions, it generally takes __ ____ ______ for the coriolis deflection to become
noticeable
Coriolis Force
Coriolis Force
Coriolis Force
- Summary
- The Coriolis Force
- is always directed
at right angles to the direction of airflow
- 90° to the
______ in NH, 90°
to the ______ in SH
- affects only wind
_________, not wind speed
- is affected by
wind ______ (stronger wind, ________ deflection)
- is strongest at
_______ and weakens ______________
Friction
- Friction acts to
_____ _____ the movement of air
- Friction
significantly influences airflow near Earth's surface (rough terrain),
but its effect becomes ____________ above a height of a few km