Energy is transformed between atoms in the radiative zone of the sun. In this layer, energy moves through the absorption and re-emission of photons by atoms. This process creates a gradient of temperature and density as energy is slowly transferred from the core to the surface of the sun.
Energy can be transferred by conduction between the Earth's lithosphere (solid outer layer) and the atmosphere (gas layer). Another example is the transfer of energy by conduction between a hot electric stove and a pot placed on it.
The Radiative Zone.
The Radiative Zone.
The convection zone.
The convection zone
In the convection Zone!
Energy is transformed between atoms in the radiative zone of the sun. In this layer, energy moves through the absorption and re-emission of photons by atoms. This process creates a gradient of temperature and density as energy is slowly transferred from the core to the surface of the sun.
Energy can be transferred by conduction between the Earth's lithosphere (solid outer layer) and the atmosphere (gas layer). Another example is the transfer of energy by conduction between a hot electric stove and a pot placed on it.
The Radiative Zone.
The Radiative Zone.
The convection zone.
the azone layer
The Radiative Zone.
The Radiative Zone.
The Radiative Zone.
The Radiative Zone.