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Atmospheric layer 
layer of gases 
Atmosphere 
-protects life on earth 
-blanket of air 
-reaches to approximately 1000 km
-consists of 78% nitrogen, 21% 
oxygen, and 1% of other gases 
(helium, neon, and ozone) 
-nitrogen 
-oxygen 
-argon
Exosphere 
STRUCTURE OF THE ATMOSPHERE
1. Exosphere 
- outermost layer of Earth's 
atmosphere 
- merges with the emptiness of 
outer space 
- hydrogen and helium
2. Thermosphere 
- second-highest layer of Earth's 
atmosphere 
- lower part contains the 
thermosphere 
- completely cloudless and free of 
water vapor 
- high as 1,727˚C
3.Mesosphere 
- third highest layer of Earth's 
atmosphere 
- coldest place on earth 
- mesopause separates the 
mesosphere from the next layer 
- low as -93˚C
4. Stratosphere 
- the second-lowest layer of Earth's 
atmosphere 
- dry, clean, cold and less dense 
- contains the ozone layer 
- temperatures rise with increasing 
altitude 
- increases gradually to -3˚C
5. Troposphere 
- lowest layer of Earth's atmosphere 
- 17 to -52˚C 
- bounded above by the tropopause 
, a boundary marked by stable 
temperatures 
- temperature usually declines with 
increasing altitude
Other layers : 
•Ozone layer - contained within the 
stratosphere 
- in the lower portion of the 
stratosphere 
•Ionosphere - region of the atmosphere 
that is ionized by solar radiation 
- overlaps the atmosphere
Greenhouse Effect 
- capture and recycle energy 
- water vapor, carbon dioxide, 
methane, nitrous oxide, 
troposheric ozone, fluorocarbons
Weather and Climate 
Weather – specific condition of the 
atmosphere over a short period of time 
- temperature, humidity, 
precipitation, cloudiness, visibility, 
wind 
Climate – general pattern of the weather
Weather Patterns and 
Irregularities 
1) Global Winds - uneven heating 
produces global circulation patterns 
2) Air Masses - drive large bodies of air 
3) Fronts - location where two air 
masses
4) Jet Streams - high in the 
atmosphere, narrow bands of 
strong wind 
5) Coriolis Effect - global winds do 
not move in straight lines

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The Atmosphere

  • 1.
  • 2. Atmospheric layer layer of gases Atmosphere -protects life on earth -blanket of air -reaches to approximately 1000 km
  • 3. -consists of 78% nitrogen, 21% oxygen, and 1% of other gases (helium, neon, and ozone) -nitrogen -oxygen -argon
  • 4. Exosphere STRUCTURE OF THE ATMOSPHERE
  • 5. 1. Exosphere - outermost layer of Earth's atmosphere - merges with the emptiness of outer space - hydrogen and helium
  • 6. 2. Thermosphere - second-highest layer of Earth's atmosphere - lower part contains the thermosphere - completely cloudless and free of water vapor - high as 1,727˚C
  • 7. 3.Mesosphere - third highest layer of Earth's atmosphere - coldest place on earth - mesopause separates the mesosphere from the next layer - low as -93˚C
  • 8. 4. Stratosphere - the second-lowest layer of Earth's atmosphere - dry, clean, cold and less dense - contains the ozone layer - temperatures rise with increasing altitude - increases gradually to -3˚C
  • 9. 5. Troposphere - lowest layer of Earth's atmosphere - 17 to -52˚C - bounded above by the tropopause , a boundary marked by stable temperatures - temperature usually declines with increasing altitude
  • 10. Other layers : •Ozone layer - contained within the stratosphere - in the lower portion of the stratosphere •Ionosphere - region of the atmosphere that is ionized by solar radiation - overlaps the atmosphere
  • 11. Greenhouse Effect - capture and recycle energy - water vapor, carbon dioxide, methane, nitrous oxide, troposheric ozone, fluorocarbons
  • 12. Weather and Climate Weather – specific condition of the atmosphere over a short period of time - temperature, humidity, precipitation, cloudiness, visibility, wind Climate – general pattern of the weather
  • 13. Weather Patterns and Irregularities 1) Global Winds - uneven heating produces global circulation patterns 2) Air Masses - drive large bodies of air 3) Fronts - location where two air masses
  • 14. 4) Jet Streams - high in the atmosphere, narrow bands of strong wind 5) Coriolis Effect - global winds do not move in straight lines