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By - Radhika Sharad Chavan.
Greenhouse Effect
CONTENTS
• Atmosphere
• Key terms
• Gases
• Causes
• Effects
ATMOSPHERE
Exosphere
Thermosphere
Mesosphere
Stratosphere
Troposphere
TROPOSPHERE
Lowest portion of earth’s atmosphere
• 75% of the entire atmosphere mass
- Water vapor
- Aerosols
• 0 km – 10 km depth ~ 10 km
• Warmer nearest earth
• Colder the further you go
Travel back to the atmosphere
STRATOSPHERE
• Second layer of earth’s atmosphere
• 10 km – 50 km depth ~ 40 km
• Colder nearer the earth surface
• Warmer the further into the atmosphere
• Energy is transferred via heat absorption
by the ozone layer.
• Heating caused by conduction from
above and convection from below.
Travel back to the atmosphere
MESOSPHERE
• Middle layer of earth’s atmosphere
• 50 km – 90 km depth ~ 40 km
• Warmer closer to earth’s surface
• Colder the further you out you go
• This is where meteors burn as they
collide with gas particles
• Most poorly understood part of the
atmosphere
Travel back to the atmosphere
THERMOSPHERE
• 4th layer of earth’s atmosphere
• 80 km – 500 km depth ~ 420 km
• Colder near earth’s surface
• Warmer as you go further into
thermosphere
• This layer absorbs radiation which in
turn electrically charge particles.
Travel back to the atmosphere
EXOSPHERE
• Outer layer of the atmosphere
• 500 km – 10,000 km depth ~ 9,500 km
• Only layer of atmosphere where gases can
escape
• Main gases found here:
- Hydrogen
- Helium
- Carbon dioxide
Travel back to the atmosphere
Thermosphere
Exosphere
Mesosphere
Stratosphere
Troposphe
re
KEY TERMS
• Condensation - process by which gas or vapor changes into a
liquid or solid
• Evaporation - the process by which a liquid changes into a gas
• Convection - upward movement of heat or other atmospheric
properties within the atmosphere
• Photosynthesis – the synthesis of complex organic materials from
carbon dioxide, water, and inorganic salts using light as an energy
source
• Radiation – energy that is transmitted in the form of rays
• Conduction – spontaneous transfer of energy through matter,
from a region of higher temperature to a region of lower
temperature
GASES
• CO2 - carbon dioxide
• MH4 - methane
• O2 – oxygen gas
• O3 - ozone
• N2 – nitrogen gas
• Ar – argon gas
• H2 – hydrogen gas
• He - helium
INCREASE IN CO2
• Increased by the burning of fossil
fuels- coal, oil, and gas
• Too much is harmful to our planet
• Creates a cycle of
carbon dioxide
within our atmosphere
• Contributes to the
hole in the ozone
layer
CARBON DIOXIDE CYCLE
3-D IMAGE OF THE OZONE HOLE
OZONE LAYER
• Three oxygen atoms bonded
together
• Forms a layer above earth that
protects us from harmful UVA
UVB rays
• The ozone hole is a depletion of
the ozone in the atmosphere.
WHAT IS CAUSING THINNING OZONE HOLE ?
• Cars
• Factories
• Pollution
• Deforestation
POLLUTANTS
EFFECTS
• Climate change
• Harms animals’ habitats
• Decrease crop production
• Flooding
• Drought
• Hurricanes
THANK YOU

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Greenhouse Effect.pptx

  • 1. By - Radhika Sharad Chavan. Greenhouse Effect
  • 2. CONTENTS • Atmosphere • Key terms • Gases • Causes • Effects
  • 4. TROPOSPHERE Lowest portion of earth’s atmosphere • 75% of the entire atmosphere mass - Water vapor - Aerosols • 0 km – 10 km depth ~ 10 km • Warmer nearest earth • Colder the further you go Travel back to the atmosphere
  • 5. STRATOSPHERE • Second layer of earth’s atmosphere • 10 km – 50 km depth ~ 40 km • Colder nearer the earth surface • Warmer the further into the atmosphere • Energy is transferred via heat absorption by the ozone layer. • Heating caused by conduction from above and convection from below. Travel back to the atmosphere
  • 6. MESOSPHERE • Middle layer of earth’s atmosphere • 50 km – 90 km depth ~ 40 km • Warmer closer to earth’s surface • Colder the further you out you go • This is where meteors burn as they collide with gas particles • Most poorly understood part of the atmosphere Travel back to the atmosphere
  • 7. THERMOSPHERE • 4th layer of earth’s atmosphere • 80 km – 500 km depth ~ 420 km • Colder near earth’s surface • Warmer as you go further into thermosphere • This layer absorbs radiation which in turn electrically charge particles. Travel back to the atmosphere
  • 8. EXOSPHERE • Outer layer of the atmosphere • 500 km – 10,000 km depth ~ 9,500 km • Only layer of atmosphere where gases can escape • Main gases found here: - Hydrogen - Helium - Carbon dioxide Travel back to the atmosphere
  • 10. KEY TERMS • Condensation - process by which gas or vapor changes into a liquid or solid • Evaporation - the process by which a liquid changes into a gas • Convection - upward movement of heat or other atmospheric properties within the atmosphere • Photosynthesis – the synthesis of complex organic materials from carbon dioxide, water, and inorganic salts using light as an energy source • Radiation – energy that is transmitted in the form of rays • Conduction – spontaneous transfer of energy through matter, from a region of higher temperature to a region of lower temperature
  • 11. GASES • CO2 - carbon dioxide • MH4 - methane • O2 – oxygen gas • O3 - ozone • N2 – nitrogen gas • Ar – argon gas • H2 – hydrogen gas • He - helium
  • 12. INCREASE IN CO2 • Increased by the burning of fossil fuels- coal, oil, and gas • Too much is harmful to our planet • Creates a cycle of carbon dioxide within our atmosphere • Contributes to the hole in the ozone layer
  • 14. 3-D IMAGE OF THE OZONE HOLE
  • 15. OZONE LAYER • Three oxygen atoms bonded together • Forms a layer above earth that protects us from harmful UVA UVB rays • The ozone hole is a depletion of the ozone in the atmosphere.
  • 16. WHAT IS CAUSING THINNING OZONE HOLE ? • Cars • Factories • Pollution • Deforestation
  • 18. EFFECTS • Climate change • Harms animals’ habitats • Decrease crop production • Flooding • Drought • Hurricanes