BY- GEOLOGICA
ATMOSPHERE
AND IT`S
STRUCTURE
ATMOSPHEERE – The atmosphere is
a thick gaseous envelope which
sorrounds the earth from all sides and
is attached to the earth`s surface by
gravitational force.
The atmosphere is
composed of –
1. Gases
2. Vapour
3. Particulates
Structure of the
atmosphere
structurally atmosphere
is divided into 4 parts .
1.Troposphere
2.Stratosphere
3.Mesosphere
4.Thermosphere
1. TROPOSPHERE-
• Lowermost layer with all weather phenomenon.
• Temperature decreases with increasing height at
the rate of 6.5*/km, is called normal lapse rate.
• The average height of the troposphere changes
from equator towards poles (decreases).
• Average height of tropsphere is about 16km.
TROPAUSE -
• Upper limit of the troposphere is called tropause.
• Tropause is about 1.5 km thick.
• Troposphere is called zone of mxing while
•The tropause is called zone of mixing stop.
2. STRATOSPHERE -
• Above the tropopause with less weather
phenomenon.
• Temperature increases and becomes 0*c at
50km.
• It is divided into two parts ozonosphere
(17-35km ) an dremaining part (35-50).
STRATOPAUSE -
• Upper limit of the tstratosphere is called
stratopause.
3. MESOOSPHERE -
• Temp. starts decreasing and becomes -80* at
it`s upper limit.
• It extends between 50-80 km.
MESOPAUSE -
• Upper limit of the mesosphere is called
mesopause.
4. THERMOSPHERE-
• Temperature increases rapidly and becomes
1700*c at it`s upper limit.
• In this region we are unable to measure the
temperature by ordinary thermometer because
of extremely low density.
• Extends from 80-640km.
• In the ionosphere we found D(60-99km),
E(99-150),F (150-380)& G (400-above) layers.
IONOSPHERE -
EXOSPHERE -
• This is the uppermost layer extending beyond 640km
Atmosphere
Atmosphere

Atmosphere

  • 1.
  • 2.
    ATMOSPHEERE – Theatmosphere is a thick gaseous envelope which sorrounds the earth from all sides and is attached to the earth`s surface by gravitational force.
  • 3.
    The atmosphere is composedof – 1. Gases 2. Vapour 3. Particulates
  • 4.
    Structure of the atmosphere structurallyatmosphere is divided into 4 parts . 1.Troposphere 2.Stratosphere 3.Mesosphere 4.Thermosphere
  • 5.
    1. TROPOSPHERE- • Lowermostlayer with all weather phenomenon. • Temperature decreases with increasing height at the rate of 6.5*/km, is called normal lapse rate. • The average height of the troposphere changes from equator towards poles (decreases). • Average height of tropsphere is about 16km. TROPAUSE - • Upper limit of the troposphere is called tropause. • Tropause is about 1.5 km thick. • Troposphere is called zone of mxing while •The tropause is called zone of mixing stop.
  • 6.
    2. STRATOSPHERE - •Above the tropopause with less weather phenomenon. • Temperature increases and becomes 0*c at 50km. • It is divided into two parts ozonosphere (17-35km ) an dremaining part (35-50). STRATOPAUSE - • Upper limit of the tstratosphere is called stratopause.
  • 7.
    3. MESOOSPHERE - •Temp. starts decreasing and becomes -80* at it`s upper limit. • It extends between 50-80 km. MESOPAUSE - • Upper limit of the mesosphere is called mesopause.
  • 8.
    4. THERMOSPHERE- • Temperatureincreases rapidly and becomes 1700*c at it`s upper limit. • In this region we are unable to measure the temperature by ordinary thermometer because of extremely low density. • Extends from 80-640km. • In the ionosphere we found D(60-99km), E(99-150),F (150-380)& G (400-above) layers. IONOSPHERE - EXOSPHERE - • This is the uppermost layer extending beyond 640km