How is energy transferred within the earth's atmosphere?

Energy is transferred within the Earth's atmosphere primarily through three processes: conduction, convection, and radiation. Conduction occurs when heat is transferred through direct contact between molecules, while convection involves the movement of air in currents, carrying heat as warmer air rises and cooler air sinks. Radiation, on the other hand, involves the transfer of energy through electromagnetic waves, such as sunlight warming the Earth's surface. These processes collectively help regulate temperature and weather patterns in the atmosphere.