atmospheric stability
DESCRIPTION
Atmospheric Stability. The resistance of the atmosphere to vertical motion. Stable air resists vertical motion Unstable air encourages vertical motion. ↓ pressure (expansion) ↑ volume = cooling. Air Falling. Air Rising. ↑ pressure (compression) ↓ volume = warming. - PowerPoint PPT PresentationTRANSCRIPT
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Atmospheric Stability
• The resistance of the atmosphere to vertical motion.
• Stable air resists vertical motion• Unstable air encourages vertical motion
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↓ pressure(expansion)↑ volume= cooling
AirRising
AirFalling
↑ pressure(compression)↓ volume= warming
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Dry adiabatic lapse rate (unsaturated air)
• Lapse rate – change in temperature with elevation
• Adiabatic process: - No heat is gained or lost by mixing with the surrounding air (“parcels of air”)
• Dry adiabatic lapse rate = 5.5°F/1000 ft
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Moist-adiabatic Rate(saturated air)
• Air rises and cools – if dew point reached, condensation occurs
• Energy released with condensation → warming• Lapse rate reduced to 3°F/1,000 ft• Parcel becomes warmer than surrounding air –
continues to rise (free convection)• Eventually reaches colder air aloft – cools and
stabilizes at new level
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Moist adiabatic lapse rate - May become unstable if air becomes warmer than surrounding area and continues to rise
Dry adiabatic lapse rate (stable)- resists vertical motion- parcel will remain in position
Inversion
Super adiabatic lapse rate- Lapse rate > dry-adiabatic rate- Example: Strong heating of ground surface- Warm air below cool air
SOUNDING – Atmospheric Temperature
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How is air lifted in the atmosphere? • Thermal lifting (convection)• Orographic lifing• Frontal lifting
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What is the stability of the air?
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What is the stability of the air?
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TTYP
• Read the material independently (2 min)• One person explains the material – the other
person listens (3 min)• The “listener” adds to the explanation any
information that they believe would help to improve their understanding of it. (2 min)
• Both people decide on the best explanation that they both agree with. (2 min)
• Both should be prepared to share the information with the entire class.
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Night Inversion
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• Air near Earth’s surface cools at night (radiation, conduction, convection)
• Cold air flows downward• Layer of warm air above = thermal belt• Inversions strongest when atmospheric conditions =
stable, calm– Clouds & water vapor reduce outgoing radiation– Wind causes air layers to mix
• Surface heating during day – cause inversion to break = severe fire conditions
Night inversion
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Marine inversion
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Subsidence Inversion
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Subsidence & mountain waves(& foehn winds)
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Signs of a Stable Atmosphere
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Signs of an Unstable Atmosphere
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Night Inversion Marine inversion
Subsidence Inversion
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Subsidence & mountain waves (& foehn winds)
Signs of a Stable Atmosphere Signs of an Unstable Atmosphere