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CH. 19: Air Pressure

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CH. 19: Air Pressure & Wind Air Pressure=the pressure exerted by the weight of air above. Air pressure is very important factor in predicting the weather! – PowerPoint PPT presentation

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Title: CH. 19: Air Pressure


1
CH. 19 Air Pressure Wind
  • Air Pressurethe pressure exerted by the weight
    of air above.
  • Air pressure is very important factor in
    predicting the weather!
  • Air pressure at sea level is 14.7 lbs per square
    inch.

2
Barometerinstrument used to measure air pressure.
  • 2 TYPES
  • 1. Aneroidcanister like device, pressure
    changes on the spring move the arrow
  • 2. Mercuryliquid device, pressure changes make
    the liquid go up(high) go down(low)

3
What causes wind?
  • Wind is the horizontal movement of air.
  • Wind is caused by the horizontal differences in
    air pressure.
  • The differences in air pressure are in turn
    caused by differences in temperature(solar
    radiation)

4
3 Factors Affecting Wind
  • 1. Pressure Differencesgreater the difference
    the greater the wind.
  • Air moves from high to low pressures
  • Isobarslines of equal pressure
  • Closely packed windy
  • Widely spaced not as windy
  • Pressure Gradientsteep means windy
  • Pressure Gradientweak/not steep means Not windy

5
  • 2. Coriolis EffectEarths rotation affects
    moving objects
  • --Free moving objects move to the
    right in the northern hemisphere
  • to the left in the southern.
  • Frictiononly important near Earth.
  • Friction slows wind can change wind direction.
  • JET STREAMShigh up fast moving!

6
19.2 Pressure Centers Wind
  • Pressure Centershelp 2 predict weather (2)
  • Low (Cyclones) air is unstable rises, cools,
    condenses, clouds stormy, cloudy, air moves ccw
    in N. hemisphere, winds move inward (?) Pressure
    decreases toward center
  • High (Anti-Cyclones) air is stable descends,
    warms, evaporates, clear/fair, air moves cw in N.
    hemisphere, winds move outward (?)
  • Pressure increases toward center

7
GLOBAL WINDS (read pgs 540-542)
  • 0 degrees equatorial low
  • 30 degrees subtropical high
  • 60 degrees subpolar low
  • 90 degrees polar high

8
  • Trade Winds belt between 0 30
  • Prevailing Westerliesbelt between 30 60
  • Polar Easterliesbelt between 60 90
  • What is the polar front? Page 541
  • What are monsoons? Page 542

9
19.3 Regional Wind Systems
  • Local Windssmall-scale winds are produced by a
    locally generated pressure gradient.
  • Local Windsare caused by 2 things
  • 1. by topographic effects (mtns. Etc.)
  • 2. by variations in surface composition
  • (land or water, etc.)

10
4 Types of Local Winds
  • 1. Sea Breezehappens during the day, land heats
    up quicker causes air to rise allowing cooler
    air to come from the sea.
  • 2. Land Breezehappens during the night, land
    cools of quicker causes the warmer air over the
    sea to rise allowing cooler air to come from the
    land.

11
  • 3. Valley Breezeoccurs during the day, air
    rises from valley floors.
  • 4. Mountain Breezeoccurs at night, air sinks
    from the mountain tops toward the valley floor.

12
MEASURING WIND
  • Wind Directionwind vane, wind direction is given
    by the direction the wind is coming FROM,
    (N,S,E,or W) or sometimes given in degrees!
  • Wind Speedanemometer.
  • Wind Sockssee them at airports measure wind
    speed direction!

13
El Nino La Nina
  • Read about these phenomena carefully!
  • When do they occur?
  • Why do they occur?
  • What global/local affects occur?
  • Global ppt. Distribution?
  • Read page 548Why does it rain in some places
    more than others?
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