Geography
Geography - Atmosphere
Atmosphere is the mixture of gases surrounding a planet. The major components of atmosphere are Nitrogen (around 78%), Oxygen (around 20%), Argon (around 0.9%). The other components of the atmosphere are Carbon dioxide, Neon, Helium, Krypton, Hydrogen and Ozone. Oxygen and carbon dioxide decreases at higher altitudes. Carbon dioxide is responsible for greenhouse effect. Ozone absorbs the ultra-violet rays preventing them from reaching earth’s surface.
Layers of Atmosphere
• Troposphere
Lowermost layer of atmosphere
Weather changes occur here
Temperature decreases by 1 degree Celsius for every 165 meters of height
It extends on average about 12 Km from earth. It is higher at equator and lower at poles
• Stratosphere
It is above troposphere
It is at about 12 to 50 Km of height above earth’s surface
Temperature increases with height due to presence of ozone layer
Aeroplanes fly here as air disturbance is less here
• Mesosphere
It is above stratosphere
It is about 50 to 80 Km of height above earth’s surface
Temperature decreases with increase of height
Meteors burn in this layer
• Thermosphere
It is above mesosphere
It is about 80 to 600 Km of height above earth’s surface
It is known as ionosphere as it contains ions, the electrically charged particles
Temperature increases with height
Helps in Radio communications
Aurora borealis is seen here
International Space Station orbits here
• Exosphere
It is above thermosphere
It is the outermost layer of earth’s atmosphere
It is about 600 to 10000 Km of height above earth’s surface
The particles escape into space
Classification of Winds
• Primary winds (Prevailing winds or Planetary winds)
Constantly blow in a particular direction throughout the year
Types of Primary winds
Trade winds (tropical easterlies)
They blow from northeast in northern hemisphere and from southeast in southern hemisphere
Used by sailing ships
Westerlies
They blow from high pressure areas of 30 degrees north and south of the equator towards the poles
Polar easterlies
They are dry, cold winds that blow at the high-pressure areas of the poles
They are weak and irregular
• Secondary winds (Seasonal winds or Periodic winds)
Change direction according to seasons
Monsoon wind is a seasonal wind that reverses direction between summer and winter
• Tertiary winds (Local winds)
Blow during a particular period in a particular area
Blow due to difference in air pressure or temperature of a location
Wind that blows from land to sea is known as land breeze and from sea to land sea breeze
Mountain slopes get cooled in the night and the dense air that blows into the valley is mountain breeze
Mountain slopes get warmed up in the day and the wind that blows upslope is valley breeze