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Air pressure and winds

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Chapter 8 FIGURE 8.4 Diurnal surface pressure changes in the middle latitudes and in the tropics. FIGURE 8.5 Atmospheric pressure in inches of mercury and in millibars. – PowerPoint PPT presentation

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Title: Air pressure and winds


1
Air pressure and winds
  • Chapter 8

2
Atmospheric Pressure
  • What causes air pressure to change in the
    horizontal?
  • Why does the air pressure change at the surface?

3
Atmospheric Pressure
  • Horizontal Pressure Variations
  • It takes a shorter column of dense, cold air to
    exert the same pressure as a taller column of
    less dense, warm air
  • A Warm air column is normally associated with a
    low surface pressure
  • A Cold air column is normally associated with a
    High surface pressure
  • At surface, horizontal difference in temperature
    horizontal pressure in pressure wind

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Atmospheric Pressure
  • Special Topic Gas Law
  • P is proportional to T x ?
  • P pressure
  • T temperature
  • ? density

http//www.youtube.com/watch?v17wGIdMvJfM
(youtube video of gas law)
7
Atmospheric Pressure
  • Daily Pressure Variations
  • Thermal tides in the tropics
  • Mid-latitude pressure variation driven by
    transitory pressure cells
  • Pressure Measurements
  • Barometer, barometric pressure
  • Standard atmospheric pressure 1013.25mb
  • Aneroid barometers
  • Altimeter, barograph

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Atmospheric Pressure
  • Pressure Readings
  • Instrument error temperature, surface tension
  • Altitude corrections high altitude add pressure,
    10mb/100m above sea level

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To get sea level pressure Add 10 mb
(elevation/ 100 m) to the station pressure
measurement. Example A station at 700 meters
elevation records a pressure of 940 mb. The sea
level pressure for this station would be 940 mb
70 mb 1010 mb
16
Surface and Upper Level Charts
  • Sea-level pressure chart constant height
  • Upper level or isobaric chart constant pressure
    surface (i.e. 500mb)
  • High heights correspond to higher than normal
    pressures at a given latitude and vice versa

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