Title: Atmospheric Pressure and Wind
1Atmospheric Pressureand Wind
- Atmospheric Circulation
- Air Pressure
- Air Pressure and Temperature
- Measurement of Pressure
- Pressure Gradient
- The Sea Breeze
- Chapters 6.0 6.1 7.0 7.1
2Atmospheric Circulation
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- The atmospheric circulation is concerned with the
large-scale air flow patterns of the whole Earth - In addition to providing our winds, the general
circulation serves to redistribute latitudinal
imbalances of energy and moisture
3Atmospheric Circulation
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Relates to Figure 7.3
Strahler and Strahler Introducing Physical
Geography
4Atmospheric Circulation
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- The atmospheric circulation is responsible for
the transfer of approximately 60 65 of the
energy from the equator to the poles
5Air Pressure
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- The force exerted by the weight of a column of
air above a given point - Air pressure is proportional to density
- High density, then high air pressure
- Low density, then low air pressure
- Air pressure decreases with an increase in
altitude
6Air Pressure
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Not in Book
7Air Pressure
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Not in Book
8Air Pressure and Temperature
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- Air pressure is also proportional to air
temperature - Cold air is denser, and has higher air pressure
- Warmer air is less dense, and has lower air
pressure
9Air Pressure and Temperature
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- High air pressure is associated with lower
temperatures - Low air pressure is associated with higher
temperatures
10Measurements of Pressure
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- Air pressure is measured by an instrument called
a barometer
11The Barometer
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Not in Book
12Measurements of Pressure
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- In climatology, air pressure is typically
expressed in millibars - A line on a map connecting equal areas of
pressure is an isobar
13Measurements of Pressure
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Figure 6.1.a
14Measurements of Pressure
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Not in Book
15Measurements of Pressure
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Not in Book
16Pressure Gradient
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- A pressure gradient is the amount of pressure
change occurring over a given distance - Air tends to mover from areas of high pressure to
areas of low pressure, until the air pressures
are equal
17Pressure Gradient
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Not in Book
18The Sea Breeze
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- An example to illustrate how temperature
differences can generate a pressure gradient, and
thereby create winds.
19The Sea Breeze
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Not in Book
20The Sea Breeze
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Not in Book
21The Sea Breeze
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Not in Book
22The Sea Breeze
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- Some main points
- Temperature variations created pressure
differences - The pressure differences initiated the flow of
wind
23The Sea Breeze
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- A sea breeze is a small-scale analogy of
larger-scale processes - Horizontal pressure gradient is the driving force
of wind
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