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How many Way’s of heat transfer in the Atmosphere? – Geography – Free PDF Download


  • The differential amount of sun’s energy is received by various latitudinal zones
  • On earth the primary reason behind the occurrence of season is insolation.
  • Insolation also effects wind systems, pressure systems, precipitation etc.


  • The heat transfer through conduction happens due to molecular activity in a conducting medium.
  • There is no actual movement of the medium itself.
  • Generally, denser materials like iron, water are good conductors, and lighter medium like air are bad conductors of heat.


  • Convection is the transfer of heat energy by actual transfer of matter or substance from one place to another.
  • E.g. heat transfer by convection cells in a boiling pot of water, atmosphere or oceans


  • Some heat from within the earth’s interior is processed in transferred to the surface through volcanoes, springs, and geysers.
  • However, the heat received from the interior at the ocean bottom is key to the survival of deep ocean lifeforms that depend on bacteria that grow near the volcanic vents.
  • At ocean depths, as sunlight is non-existent, photosynthesis is impossible.
  • The bacteria rely on chemosynthesis, a process in which microbes use chemicals in the vent fluid to produce energy


  • Radiation doesn’t require a medium for heat transfer.
  • Heat is transferred from one body to another without actual contact or movement in the medium. • E.g. Heat transfer from the sun to earth through space.


  • Insolation is the amount of sun’s energy received in the form of radiation by the earth.
  • It is measured as the amount of solar energy received per square centimeter per minute.
  • Earth intercepts less than a billionth of solar radiation.
  • Earth receives sun’s radiation in the form of short waves which are electromagnetic.
  • The earth absorbs short wave radiation during daytime and reflects the heat received into space as longwave radiation during night.


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