Layers of the Atmosphere. Today’s Objectives Today’s Objectives 1. Identify the layers of the...
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Transcript of Layers of the Atmosphere. Today’s Objectives Today’s Objectives 1. Identify the layers of the...
Layers of the Layers of the AtmosphereAtmosphere
Today’s ObjectivesToday’s Objectives
1. Identify the layers of the Earth’s atmosphere.
2. Describe the layers of the Earth’s atmosphere.
3. Diagram and label the layers of the atmosphere with temperature and composition.
Students will be able to:
Troposphere – 0-10 milesTroposphere – 0-10 miles• The layer we walk around in
• Most airplanes fly here
• Where most weather occurs
• Height varies due to solar energy
Low at poles, higher over equator
Troposphere – 0-10 milesTroposphere – 0-10 miles
-3.5ºF per 1000 feet (-6.4ºC per 1000 m)
• Air gets colder with altitude
• 18ºC (56ºF) at surface
• -58ºC (-50ºF) at upper limit
• ambient atmospheric lapse rate (ESL)
Tropopause – ~10 milesTropopause – ~10 miles• Divides troposphere and
stratosphere
• The height at which the temperature stops decreasing.
• Temperature can reach -70ºF
Above 90% of total atmosphere
Stratosphere – 10-30 Stratosphere – 10-30 milesmiles
Why the inversion?
• Lower limit mixes with troposphere to form the jet stream (115+ mph)
• Air gets warmer with altitude
• This is called a temperature inversion
The Ozo
ne layer
The Ozo
ne layer
Stratosphere – 10-30 Stratosphere – 10-30 milesmiles
• High concentration found around 15 miles high
• Absorbs most of the Sun’s harmful ultraviolet rays.
• Absorption raises the temperature
The Ozone layer
The Ozone layer
Stratopause – 30 milesStratopause – 30 miles• Divides stratosphere and
mesosphere
• The height temperature STOPSSTOPS increasing.
• Temperature can reach 40ºF
• 1 mb (millibar) of pressure
Above 99.9% of total atmosphere
• Again, temperature decreases as elevation increases.
• This is due to no ozone and molecules being far apart
• Can reach temperatures as low as -130ºF
Mesosphere – 30-50 Mesosphere – 30-50 milesmiles
Why?Why?
Mesopause – 50 milesMesopause – 50 miles• Divides mesosphere and
thermosphere
• The 2nd height at which the temperature stops decreasing.
• Temperature can reach -130ºF
• the “Hot Layer”
• Oxygen atoms absorb energetic solar rays, warming the air
• Reaches around 2,700ºF
Thermosphere – 50-120 Thermosphere – 50-120 milesmiles
Protects us from meteors and Protects us from meteors and obsolete satellitesobsolete satellites
• Auroras occur in this layer
Thermosphere – 50-120 Thermosphere – 50-120 milesmiles
• Upper reaches of atmosphere
• So little gravity that atoms are able to shoot off into space
• Range 570ºF to over 3,000ºF
Exosphere – 120+ milesExosphere – 120+ miles
Satellites and Space Shuttle flySatellites and Space Shuttle fly
IonosphereIonosphereNot really a layer…but a regionNot really a layer…but a region
IonosphereIonosphere
RadiosondeRadiosonde• Instrument used
to measure:
• vertical profile of air
• temperature up to ~20 mil
RadiosondeRadiosonde