Convection currents in Earth's atmosphere transport heat from the poles towards the equator .
Step-by-step explanation:
Atmospheric convection is that the results of a parcel-environment instability, or temperature distinction, layer within the atmosphere.
The liquid or gas in hot areas is a smaller amount dense than the liquid or gas in cold areas, thus it rises into the cold areas.
The denser cold liquid or gas falls into the nice and cozy areas. during this means, convection currents that transfer heat from place to position are created.