Answer:
Okay, Look at the explaination.
Step-by-step explanation:
The atmosphere is heated in several ways - heat from the core of the planet, by radiation from the Sun, conduction from contact with warm land and water, convection to even out the temperature and by absorption of actinic radiation from the nice and cozy land and water. Then, convection then spreads and evens out the warmth.
I really hope this helps!