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Composition and
Layers of the Atmosphere
Mixture of gases
surrounding the earth
Held by the gravitational
field
“gaseous envelope” of the
Earth
Troposhere
Stratosphere – Ozone Layer
Mesosphere
Thermosphere –
Ionosphere
Exosphere
Magnetoshpere
 lowest layer of the earth's
atmosphere and site of all
weather on the earth. The
troposphere is bounded on
the top by a layer of air
called the tropopause, which
separates the troposphere
from the stratosphere, and
on the bottom by the surface
of the earth.
 upper layer of the atmosphere.
 In the lower portion of the
stratosphere, the temperature
remains nearly constant with
height, but in the upper portion
the temperature increases rapidly
with height because of
absorption of sunlight by ozone.
Found in the stratosphere
Ozone concentrations (O3)
of up to 10 parts per million
occur in the ozone layer.
The ozone forms there by
the action of sunlight on
oxygen.
the layer of the Earth's
atmosphere in which
temperature
decreases rapidly.
Where meteors
disintegrate
Temperature
increases by
height
Where space
shuttles fly by
Auroral displays
 the air is extremely thin, having
about the density of the gas in a
vacuum tube.
 When the atmospheric particles are
ionized by ultraviolet radiation from
the Sun or by other radiation, they
tend to remain ionized, because few
collisions occur between ions.
 Reflection of signals
Outer limit of the
atmosphere
Where artificial
satellites and
space stations fly
by
region surrounding Earth
in which charged particles
are affected by the
planet’s magnetic field.
 mixture of gases that composes the
atmosphere surrounding Earth.
 The principal constituents of
the atmosphere of Earth are
nitrogen (78 percent) and
oxygen (21 percent).
 The atmospheric gases in the
remaining 1 percent are
argon, carbon dioxide, and
trace amounts of hydrogen,
ozone, methane, carbon
monoxide, helium, neon,
krypton, and xenon.
 Colorless, odorless, slightly soluble in water
 Does not combine readily with other
substances
 It is an important element in plant nutrition;
certain bacteria in the soil convert
atmospheric nitrogen into a form, such as
nitrate, that can be absorbed by plants.
 Very active
 Gas produced by plants when they make their
own food.
 It combines with iron to form rust. In
burning, oxygen in air combines with carbon
to form CO2.
 It does not combine easily with other
substances
 Produced by animals, burning of fuels, and by
volcanic eruptions
 Absorbed by plants and changed into food.
 Air near the ground has more CO2 and is
therefore warmer than air far above.
 Like Argon, not reactive.
 Noble gases
 Poisonous gas
 It occurs in natural gas, as firedamp in coal
mines, as a by-product of petroleum refining,
and as a product of decomposition of matter
in swamps.
 Hydrogen is highly active, it readily combines
with other substances in the air leaving little
free hydrogen.
 Helium is the lightest noble gas. It is inactive.
Used in balloons.
 John Mayow (1600s) – two parts of air; one
part supported life and fire, the other part did
not.
 Daniel Rutherford – proved that there was
CO2 in the air which did not support life
 Joseph Priestley (1774) – discovered Oxygen
 Lord Rayleigh and William Ramsay discovered
Argon in 1894.
1. First Atmosphere: H and He
2. Second Atmosphere:
Ammonia, Methane, Water
Vapor, CO2, carbon
monoxide, and hydrogen
sulfide
3. Third Atmosphere: present
atmosphere
Atmosphere 1
Atmosphere 1

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Key note speaker Neum_Admir Softic_ENG.pdf
 

Atmosphere 1

  • 1. Composition and Layers of the Atmosphere
  • 2.
  • 3.
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  • 5. Mixture of gases surrounding the earth Held by the gravitational field “gaseous envelope” of the Earth
  • 6. Troposhere Stratosphere – Ozone Layer Mesosphere Thermosphere – Ionosphere Exosphere Magnetoshpere
  • 7.
  • 8.  lowest layer of the earth's atmosphere and site of all weather on the earth. The troposphere is bounded on the top by a layer of air called the tropopause, which separates the troposphere from the stratosphere, and on the bottom by the surface of the earth.
  • 9.  upper layer of the atmosphere.  In the lower portion of the stratosphere, the temperature remains nearly constant with height, but in the upper portion the temperature increases rapidly with height because of absorption of sunlight by ozone.
  • 10. Found in the stratosphere Ozone concentrations (O3) of up to 10 parts per million occur in the ozone layer. The ozone forms there by the action of sunlight on oxygen.
  • 11.
  • 12.
  • 13. the layer of the Earth's atmosphere in which temperature decreases rapidly. Where meteors disintegrate
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  • 16.  the air is extremely thin, having about the density of the gas in a vacuum tube.  When the atmospheric particles are ionized by ultraviolet radiation from the Sun or by other radiation, they tend to remain ionized, because few collisions occur between ions.  Reflection of signals
  • 17.
  • 18. Outer limit of the atmosphere Where artificial satellites and space stations fly by
  • 19. region surrounding Earth in which charged particles are affected by the planet’s magnetic field.
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  • 23.
  • 24.  mixture of gases that composes the atmosphere surrounding Earth.
  • 25.  The principal constituents of the atmosphere of Earth are nitrogen (78 percent) and oxygen (21 percent).  The atmospheric gases in the remaining 1 percent are argon, carbon dioxide, and trace amounts of hydrogen, ozone, methane, carbon monoxide, helium, neon, krypton, and xenon.
  • 26.
  • 27.  Colorless, odorless, slightly soluble in water  Does not combine readily with other substances  It is an important element in plant nutrition; certain bacteria in the soil convert atmospheric nitrogen into a form, such as nitrate, that can be absorbed by plants.
  • 28.  Very active  Gas produced by plants when they make their own food.  It combines with iron to form rust. In burning, oxygen in air combines with carbon to form CO2.
  • 29.  It does not combine easily with other substances
  • 30.  Produced by animals, burning of fuels, and by volcanic eruptions  Absorbed by plants and changed into food.  Air near the ground has more CO2 and is therefore warmer than air far above.
  • 31.  Like Argon, not reactive.  Noble gases
  • 32.  Poisonous gas  It occurs in natural gas, as firedamp in coal mines, as a by-product of petroleum refining, and as a product of decomposition of matter in swamps.
  • 33.  Hydrogen is highly active, it readily combines with other substances in the air leaving little free hydrogen.  Helium is the lightest noble gas. It is inactive. Used in balloons.
  • 34.  John Mayow (1600s) – two parts of air; one part supported life and fire, the other part did not.  Daniel Rutherford – proved that there was CO2 in the air which did not support life  Joseph Priestley (1774) – discovered Oxygen  Lord Rayleigh and William Ramsay discovered Argon in 1894.
  • 35. 1. First Atmosphere: H and He 2. Second Atmosphere: Ammonia, Methane, Water Vapor, CO2, carbon monoxide, and hydrogen sulfide 3. Third Atmosphere: present atmosphere

Editor's Notes

  1. Tropo – clouds, ski, airplane Strato – ozone, weather balloon meso – meteors Exo – satellite, space station Thermo – aurora, space shuttle