A vertical air current that is generated by temperature -induced density differences is an example of heat transfer by

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A vertical air current generated by temperature-induced density differences is an example of heat transfer by convection, which involves the movement of a fluid (in this case air) due to differences in temperature and density. Diffusion (A) refers to the spontaneous movement of particles from an area of high concentration to an area of low concentration, while transmission (B) typically refers to the transfer of energy through a medium, such as light passing through glass. Conduction (C) refers to the transfer of heat through a material by direct contact, without any movement of the material itself. Advection (D) is similar to convection, but it specifically refers to the movement of a fluid due to external forces, such as wind driving ocean currents.

A Vertical Air Current That Is Generated by Temperature -Induced